Ua Pou Island, Marquesas Islands, French Polynesia, Francei
Regional Level Types | |
---|---|
Ua Pou Island | Island |
Marquesas Islands | Group of Islands |
French Polynesia | Overseas Collectivity |
France | Country |
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Locality type:
Age:
2.93 ± 0.04 to 2.35 ± 0.03 Ma
Geologic Time:
Dating method:
K-Ar
Reference for age:
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Other/historical names associated with this locality:
Ua Pu
Name(s) in local language(s):
Île de Ua Pou (ʻUapou), Îles Marquises (Archipel des Marquises; Te Henua (K)enana; Te Fenua `Enata), Polynésie française (Pōrīnetia Farāni)
Ua Pou (Ua Pu), located 50 km south of Nuku Hiva in the Marquesas northern group, is the fifth largest island of French Polynesia (105 km2). In contrast to most other Marquesas islands, it is devoid of any caldera. Ua Pou has a diamond-shaped outline and a north–south-trending central crest, circa 600 m high, from which diverge many secondary crests separated by deep valleys. The villages of Hakahau, Hakamoui, Paaumea, Hohoi, Hakatao, Hakamaii, Haakuti and Hakahetau are located in these valleys.
Ua Pou is known for its abundant and petrologically diverse phonolites (Lacroix, 1928 and 1931; Chubb, 1930; Bishop & Woolley, 1973; Brousse, 1978; Brousse & Maury, 1978; Legendre et al., 2005).
The most spectacular features of the island are its phonolitic protrusions (Ua Pou means the Pillar Island), the summits of which tower several hundred metres above the radial crests; the four highest pillars are named Oave (1203 m), Pouakei (1034 m), Matahenua (1028 m), Poumaka (979 m), and Poutetainui (970 m). The Ua Pou volcanic edifice is made up of a thick lava pile, mostly phonolitic and basaltic, intruded by about 30 phonolitic and trachytic protrusions. Like the other Marquesas islands, Ua Pou is devoid of any coral reef or reefal limestone unit.
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Rock Types Recorded
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Alphabetical List Tree DiagramDetailed Mineral List:
ⓘ Aegirine Formula: NaFe3+Si2O6 Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Aegirine-augite Formula: (NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6 Localities: Reference: Brousse R., Maury R.C. (1978): Minéralogie d'une phonolite à grenat de l'île de Ua Pou (Marquises, Pacifique central). Bulletin de Minéralogie, 101, 3–10; Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Aenigmatite Formula: Na4[Fe2+10Ti2]O4[Si12O36] Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Albite Formula: Na(AlSi3O8) Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ Albite var. Anorthoclase Formula: (Na,K)AlSi3O8 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ 'Amphibole Supergroup' Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Analcime Formula: Na(AlSi2O6) · H2O Localities: Reference: Brousse R., Maury R.C. (1978): Minéralogie d'une phonolite à grenat de l'île de Ua Pou (Marquises, Pacifique central). Bulletin de Minéralogie, 101, 3–10. |
ⓘ Andradite Formula: Ca3Fe3+2(SiO4)3 Localities: Reference: Brousse R., Maury R.C. (1978): Minéralogie d'une phonolite à grenat de l'île de Ua Pou (Marquises, Pacifique central). Bulletin de Minéralogie, 101, 3–10. |
ⓘ Andradite var. Titanium-bearing Andradite Formula: Ca3(Fe3+,Ti)2(SiO4)3 Localities: Reference: Brousse R., Maury R.C. (1978): Minéralogie d'une phonolite à grenat de l'île de Ua Pou (Marquises, Pacifique central). Bulletin de Minéralogie, 101, 3–10. |
ⓘ Anorthite Formula: Ca(Al2Si2O8) Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ 'Apatite' Formula: Ca5(PO4)3(Cl/F/OH) Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ Augite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ Augite var. Fassaite Formula: (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ Calcite Formula: CaCO3 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ 'Clinopyroxene Subgroup' Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Diopside Formula: CaMgSi2O6 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Edenite Formula: NaCa2Mg5(Si7Al)O22OH2 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ 'Fayalite-Forsterite Series' Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Forsterite Formula: Mg2SiO4 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ 'Garnet Group' Formula: X3Z2(SiO4)3 Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ 'Garnet Group var. Titanium-bearing Garnet' Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Hedenbergite Formula: CaFe2+Si2O6 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ 'Hornblende' Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ 'Iddingsite' Formula: MgO · Fe2O3 · 3SiO2 · 4H2O Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ Ilmenite Formula: Fe2+TiO3 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ Kaersutite Formula: NaCa2(Mg3AlTi4+)(Si6Al2)O22O2 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ 'K Feldspar' Formula: KAlSi3O8 Localities: Reference: Brousse R., Maury R.C. (1978): Minéralogie d'une phonolite à grenat de l'île de Ua Pou (Marquises, Pacifique central). Bulletin de Minéralogie, 101, 3–10; Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Magnetite Formula: Fe2+Fe3+2O4 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Magnetite var. Titanium-bearing Magnetite Formula: Fe2+(Fe3+,Ti)2O4 Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Nepheline Formula: Na3K(Al4Si4O16) Localities: Reference: Brousse R., Maury R.C. (1978): Minéralogie d'une phonolite à grenat de l'île de Ua Pou (Marquises, Pacifique central). Bulletin de Minéralogie, 101, 3–10; Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Sanidine Formula: K(AlSi3O8) Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Sodalite Formula: Na4(Si3Al3)O12Cl Localities: Reference: Brousse R., Maury R.C. (1978): Minéralogie d'une phonolite à grenat de l'île de Ua Pou (Marquises, Pacifique central). Bulletin de Minéralogie, 101, 3–10; Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ 'Sodic plagioclase' Reference: Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ Titanite Formula: CaTi(SiO4)O Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2 |
ⓘ 'Zeolite Group' Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
ⓘ Zircon Formula: Zr(SiO4) Reference: Legendre C., Maury R.C., Caroff M., Guillou H., Cotten J., Chauvel C., Bollinger C., Hémond C., Guille G., Blais S., Rossi P., Savanier D. (2005): Origin of exceptionally abundant phonolites on Ua Pou island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46, (9), 1925-1962. |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 4 - Oxides and Hydroxides | |||
---|---|---|---|
ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
ⓘ | var. Titanium-bearing Magnetite | 4.BB.05 | Fe2+(Fe3+,Ti)2O4 |
Group 5 - Nitrates and Carbonates | |||
ⓘ | Calcite | 5.AB.05 | CaCO3 |
Group 9 - Silicates | |||
ⓘ | Aegirine | 9.DA.25 | NaFe3+Si2O6 |
ⓘ | Aegirine-augite | 9.DA.20 | (NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6 |
ⓘ | Aenigmatite | 9.DH.40 | Na4[Fe2+10Ti2]O4[Si12O36] |
ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
ⓘ | var. Anorthoclase | 9.FA.35 | (Na,K)AlSi3O8 |
ⓘ | Analcime | 9.GB.05 | Na(AlSi2O6) · H2O |
ⓘ | Andradite | 9.AD.25 | Ca3Fe3+2(SiO4)3 |
ⓘ | var. Titanium-bearing Andradite | 9.AD.25 | Ca3(Fe3+,Ti)2(SiO4)3 |
ⓘ | Anorthite | 9.FA.35 | Ca(Al2Si2O8) |
ⓘ | Augite | 9.DA.15 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
ⓘ | var. Fassaite | 9.DA.15 | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
ⓘ | Diopside | 9.DA.15 | CaMgSi2O6 |
ⓘ | Edenite | 9.DE.15 | NaCa2Mg5(Si7Al)O22OH2 |
ⓘ | Forsterite | 9.AC.05 | Mg2SiO4 |
ⓘ | Hedenbergite | 9.DA.15 | CaFe2+Si2O6 |
ⓘ | Kaersutite | 9.DE.15 | NaCa2(Mg3AlTi4+)(Si6Al2)O22O2 |
ⓘ | Nepheline | 9.FA.05 | Na3K(Al4Si4O16) |
ⓘ | Sanidine | 9.FA.30 | K(AlSi3O8) |
ⓘ | Sodalite | 9.FB.10 | Na4(Si3Al3)O12Cl |
ⓘ | Titanite | 9.AG.15 | CaTi(SiO4)O |
ⓘ | 'Zeolite Group' | 9.G0. | |
ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
Unclassified Minerals, Rocks, etc. | |||
ⓘ | 'Amphibole Supergroup' | - | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
ⓘ | 'Apatite' | - | Ca5(PO4)3(Cl/F/OH) |
ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
ⓘ | 'Clinopyroxene Subgroup' | - | |
ⓘ | 'Fayalite-Forsterite Series' | - | |
ⓘ | 'Garnet Group' | - | X3Z2(SiO4)3 |
ⓘ | 'var. Titanium-bearing Garnet' | - | X3Z2(SiO4)3 |
ⓘ | 'Hornblende' | - | |
ⓘ | 'Iddingsite' | - | MgO · Fe2O3 · 3SiO2 · 4H2O |
ⓘ | 'K Feldspar' | - | KAlSi3O8 |
ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
ⓘ | 'Sodic plagioclase' | - |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
H | ⓘ Edenite | NaCa2Mg5(Si7Al)O22OH2 |
H | ⓘ Iddingsite | MgO · Fe2O3 · 3SiO2 · 4H2O |
H | ⓘ Analcime | Na(AlSi2O6) · H2O |
H | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
C | Carbon | |
C | ⓘ Calcite | CaCO3 |
O | Oxygen | |
O | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
O | ⓘ Ilmenite | Fe2+TiO3 |
O | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
O | ⓘ K Feldspar | KAlSi3O8 |
O | ⓘ Magnetite var. Titanium-bearing Magnetite | Fe2+(Fe3+,Ti)2O4 |
O | ⓘ Titanite | CaTi(SiO4)O |
O | ⓘ Nepheline | Na3K(Al4Si4O16) |
O | ⓘ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
O | ⓘ Sodalite | Na4(Si3Al3)O12Cl |
O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
O | ⓘ Zircon | Zr(SiO4) |
O | ⓘ Forsterite | Mg2SiO4 |
O | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
O | ⓘ Diopside | CaMgSi2O6 |
O | ⓘ Hedenbergite | CaFe2+Si2O6 |
O | ⓘ Anorthite | Ca(Al2Si2O8) |
O | ⓘ Albite | Na(AlSi3O8) |
O | ⓘ Kaersutite | NaCa2(Mg3AlTi4+)(Si6Al2)O22O2 |
O | ⓘ Edenite | NaCa2Mg5(Si7Al)O22OH2 |
O | ⓘ Calcite | CaCO3 |
O | ⓘ Iddingsite | MgO · Fe2O3 · 3SiO2 · 4H2O |
O | ⓘ Albite var. Anorthoclase | (Na,K)AlSi3O8 |
O | ⓘ Analcime | Na(AlSi2O6) · H2O |
O | ⓘ Andradite var. Titanium-bearing Andradite | Ca3(Fe3+,Ti)2(SiO4)3 |
O | ⓘ Magnetite | Fe2+Fe23+O4 |
O | ⓘ Andradite | Ca3Fe23+(SiO4)3 |
O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
O | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
O | ⓘ Sanidine | K(AlSi3O8) |
O | ⓘ Aenigmatite | Na4[Fe102+Ti2]O4[Si12O36] |
O | ⓘ Aegirine | NaFe3+Si2O6 |
O | ⓘ Garnet Group | X3Z2(SiO4)3 |
F | Fluorine | |
F | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
F | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Na | Sodium | |
Na | ⓘ Nepheline | Na3K(Al4Si4O16) |
Na | ⓘ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
Na | ⓘ Sodalite | Na4(Si3Al3)O12Cl |
Na | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
Na | ⓘ Albite | Na(AlSi3O8) |
Na | ⓘ Kaersutite | NaCa2(Mg3AlTi4+)(Si6Al2)O22O2 |
Na | ⓘ Edenite | NaCa2Mg5(Si7Al)O22OH2 |
Na | ⓘ Albite var. Anorthoclase | (Na,K)AlSi3O8 |
Na | ⓘ Analcime | Na(AlSi2O6) · H2O |
Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Na | ⓘ Aenigmatite | Na4[Fe102+Ti2]O4[Si12O36] |
Na | ⓘ Aegirine | NaFe3+Si2O6 |
Mg | Magnesium | |
Mg | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Mg | ⓘ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Mg | ⓘ Forsterite | Mg2SiO4 |
Mg | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
Mg | ⓘ Diopside | CaMgSi2O6 |
Mg | ⓘ Kaersutite | NaCa2(Mg3AlTi4+)(Si6Al2)O22O2 |
Mg | ⓘ Edenite | NaCa2Mg5(Si7Al)O22OH2 |
Mg | ⓘ Iddingsite | MgO · Fe2O3 · 3SiO2 · 4H2O |
Al | Aluminium | |
Al | ⓘ K Feldspar | KAlSi3O8 |
Al | ⓘ Nepheline | Na3K(Al4Si4O16) |
Al | ⓘ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
Al | ⓘ Sodalite | Na4(Si3Al3)O12Cl |
Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Al | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
Al | ⓘ Anorthite | Ca(Al2Si2O8) |
Al | ⓘ Albite | Na(AlSi3O8) |
Al | ⓘ Kaersutite | NaCa2(Mg3AlTi4+)(Si6Al2)O22O2 |
Al | ⓘ Edenite | NaCa2Mg5(Si7Al)O22OH2 |
Al | ⓘ Albite var. Anorthoclase | (Na,K)AlSi3O8 |
Al | ⓘ Analcime | Na(AlSi2O6) · H2O |
Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Al | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Al | ⓘ Sanidine | K(AlSi3O8) |
Si | Silicon | |
Si | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Si | ⓘ K Feldspar | KAlSi3O8 |
Si | ⓘ Titanite | CaTi(SiO4)O |
Si | ⓘ Nepheline | Na3K(Al4Si4O16) |
Si | ⓘ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
Si | ⓘ Sodalite | Na4(Si3Al3)O12Cl |
Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Si | ⓘ Zircon | Zr(SiO4) |
Si | ⓘ Forsterite | Mg2SiO4 |
Si | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
Si | ⓘ Diopside | CaMgSi2O6 |
Si | ⓘ Hedenbergite | CaFe2+Si2O6 |
Si | ⓘ Anorthite | Ca(Al2Si2O8) |
Si | ⓘ Albite | Na(AlSi3O8) |
Si | ⓘ Kaersutite | NaCa2(Mg3AlTi4+)(Si6Al2)O22O2 |
Si | ⓘ Edenite | NaCa2Mg5(Si7Al)O22OH2 |
Si | ⓘ Iddingsite | MgO · Fe2O3 · 3SiO2 · 4H2O |
Si | ⓘ Albite var. Anorthoclase | (Na,K)AlSi3O8 |
Si | ⓘ Analcime | Na(AlSi2O6) · H2O |
Si | ⓘ Andradite var. Titanium-bearing Andradite | Ca3(Fe3+,Ti)2(SiO4)3 |
Si | ⓘ Andradite | Ca3Fe23+(SiO4)3 |
Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Si | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Si | ⓘ Sanidine | K(AlSi3O8) |
Si | ⓘ Aenigmatite | Na4[Fe102+Ti2]O4[Si12O36] |
Si | ⓘ Aegirine | NaFe3+Si2O6 |
Si | ⓘ Garnet Group | X3Z2(SiO4)3 |
P | Phosphorus | |
P | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
Cl | Chlorine | |
Cl | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
Cl | ⓘ Sodalite | Na4(Si3Al3)O12Cl |
Cl | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
K | Potassium | |
K | ⓘ K Feldspar | KAlSi3O8 |
K | ⓘ Nepheline | Na3K(Al4Si4O16) |
K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
K | ⓘ Albite var. Anorthoclase | (Na,K)AlSi3O8 |
K | ⓘ Sanidine | K(AlSi3O8) |
Ca | Calcium | |
Ca | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Ca | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
Ca | ⓘ Titanite | CaTi(SiO4)O |
Ca | ⓘ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
Ca | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
Ca | ⓘ Diopside | CaMgSi2O6 |
Ca | ⓘ Hedenbergite | CaFe2+Si2O6 |
Ca | ⓘ Anorthite | Ca(Al2Si2O8) |
Ca | ⓘ Kaersutite | NaCa2(Mg3AlTi4+)(Si6Al2)O22O2 |
Ca | ⓘ Edenite | NaCa2Mg5(Si7Al)O22OH2 |
Ca | ⓘ Calcite | CaCO3 |
Ca | ⓘ Andradite var. Titanium-bearing Andradite | Ca3(Fe3+,Ti)2(SiO4)3 |
Ca | ⓘ Andradite | Ca3Fe23+(SiO4)3 |
Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Ti | Titanium | |
Ti | ⓘ Ilmenite | Fe2+TiO3 |
Ti | ⓘ Magnetite var. Titanium-bearing Magnetite | Fe2+(Fe3+,Ti)2O4 |
Ti | ⓘ Titanite | CaTi(SiO4)O |
Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Ti | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
Ti | ⓘ Kaersutite | NaCa2(Mg3AlTi4+)(Si6Al2)O22O2 |
Ti | ⓘ Andradite var. Titanium-bearing Andradite | Ca3(Fe3+,Ti)2(SiO4)3 |
Ti | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Ti | ⓘ Aenigmatite | Na4[Fe102+Ti2]O4[Si12O36] |
Fe | Iron | |
Fe | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Fe | ⓘ Ilmenite | Fe2+TiO3 |
Fe | ⓘ Magnetite var. Titanium-bearing Magnetite | Fe2+(Fe3+,Ti)2O4 |
Fe | ⓘ Aegirine-augite | (NaaCabFec2+Mgd)(Fee3+AlfFeg2+Mgh)Si2O6 |
Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Fe | ⓘ Augite var. Fassaite | (Ca,Na)(Mg,Fe2+,Al,Fe3+,Ti)[(Si,Al)2O6] |
Fe | ⓘ Hedenbergite | CaFe2+Si2O6 |
Fe | ⓘ Iddingsite | MgO · Fe2O3 · 3SiO2 · 4H2O |
Fe | ⓘ Andradite var. Titanium-bearing Andradite | Ca3(Fe3+,Ti)2(SiO4)3 |
Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
Fe | ⓘ Andradite | Ca3Fe23+(SiO4)3 |
Fe | ⓘ Aenigmatite | Na4[Fe102+Ti2]O4[Si12O36] |
Fe | ⓘ Aegirine | NaFe3+Si2O6 |
Zr | Zirconium | |
Zr | ⓘ Zircon | Zr(SiO4) |
Geochronology
Mineralization age: Pliocene : 4.00 ± 0.06 MaImportant note: This table is based only on rock and mineral ages recorded on mindat.org for this locality and is not necessarily a complete representation of the geochronology, but does give an indication of possible mineralization events relevant to this locality. As more age information is added this table may expand in the future. A break in the table simply indicates a lack of data entered here, not necessarily a break in the geologic sequence. Grey background entries are from different, related, localities.
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Fossils
This region is too big to display the fossil list, try looking at smaller subregions.References
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Year (asc) Year (desc) Author (A-Z) Author (Z-A)Lacroix A. (1928): Nouvelles observations sur les laves des îles Marquises et de l'île Tubuai (Polynésie australe). Comptes Rendus de l'Académie des Sciences, 187, 397.
Lacroix A. (1931): Les phonolites néphéliniques et leucitiques de l'île Ua Pou (Archipel des Marquises). Comptes Rendus de l'Académie des Sciences, 20, 1161–1166.
Chubb L.J. (1930): The geology of the Marquesas islands. Bernice P. Bishop Museum Bullettin, 68, 1–71.
Bishop, A. C., & Woolley, A. R. (1973). A basalt-trachyte-phonolite series from Ua Pu, Marquesas islands, Pacific ocean. Contributions to Mineralogy and Petrology, 39(4), 309-326. doi.org/ 10.1007/BF00376471
Brousse R. (1978): Eléments d'analyses de quelques îles des Marquises: Fatu Hiva, Tahuata, Motane, Ua Pou. Cahiers du Pacifique, Volume Spécial ‘Marquises’, Fondation Singer-Polignac, Paris, pages 107–144.
Brousse R., Maury R.C. (1978): Minéralogie d'une phonolite à grenat de l'île de Ua Pou (Marquises, Pacifique central). Bulletin de Minéralogie, 101, 3–10.
Woolley, A. R. (2019). Alkaline Rocks and Carbonatites of the World, Part 4: Antarctica, Asia and Europe (excluding the former USSR), Australasia and Oceanic Islands. Geological Society of London, p. 534.
Legendre, C., Maury, R. C., Caroff, M., Guillou, H., Cotten, J., Chauvel, C., ... & Rossi, P. (2005). Origin of exceptionally abundant phonolites on Ua Pou Island (Marquesas, French Polynesia): Partial melting of basanites followed by crustal contamination. Journal of Petrology, 46(9), 1925-1962. doi.org/10.1093/petrology/egi043
Dupuy, C., Vidal, P., Barsczus, H. G., & Chauvel, C. (1987). Origin of basalts from the Marquesas Archipelago (south central Pacific Ocean): isotope and trace element constraints. Earth and planetary science letters, 82(1-2), 145-152. doi.org/10.1016/0012-821X(87)90114-2
Localities in this Region
- French Polynesia
- Marquesas Islands
- Ua Pou Island
- Marquesas Islands
Other Regions, Features and Areas that Intersect
Pacific PlateTectonic Plate
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Ua Pou garnet phonolites, Ua Pou Island, Marquesas Islands, French Polynesia, France