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  • (Table 16) Chemical composition of effusive rocks from the island slope of the Yap Trench
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(Table 16) Chemical composition of effusive rocks from the island slope of the Yap Trench

Fuente: PANGAEA
Salvato in:
Dettagli Bibliografici
Autori principali: Sharas'kin, Anatoly Ya, Zakariadze, Guram S, Dmitriev, Leonid V, Dobretsov, Nikolay L, Levashov, G B, Komatsu, M, Dietrich, Volker, Oberhänsli, Roland
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1980
Soggetti:
Aluminium oxide; Archive of Ocean Data; ARCOD; Barium; Boron; Calcium oxide; Carbon dioxide; Chromium; Cobalt; Copper; DM1427-D; DM1428-D; DM1429-D; DM17__Campaign; Dmitry Mendeleev; Dredge; DRG; Elevation of event; Elevation of event 2; Event label; Fluorine; Iron oxide, Fe2O3; Iron oxide, FeO; Latitude of event; Latitude of event 2; Lithium; Longitude of event; Longitude of event 2; Loss on ignition; Magnesium oxide; Manganese oxide; Nickel; Philippine Sea; Phosphorus pentoxide; Potassium oxide; Rubidium; Sample code/label; Sample type; Silicon dioxide; Sodium oxide; Strontium; Sum; Titanium dioxide; Vanadium; Water in rock; Zinc
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Accesso online

https://doi.org/10.1594/PANGAEA.736336

Documenti analoghi

  • (Table 51) Chemical composition of metamorphosed basalts, metaandesites, their breccias and tuffs from the Yap Trench and the Palau Island slope
    di: Savelyeva, G N, et al.
    Pubblicazione: (1980)
  • (Table 15) Chemical composition of effusive rocks from the intersection zone of the Mariana Trench and Yap Trench
    di: Sharas'kin, Anatoly Ya, et al.
    Pubblicazione: (1980)
  • (Table 33) Chemical composition of gabbro from the Yap Trench
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    Pubblicazione: (1980)
  • (Table 17) Chemical composition of rocks from the Palau-Kyushu Ridge of the island slope of the Palau Trench
    di: Sharas'kin, Anatoly Ya, et al.
    Pubblicazione: (1980)
  • (Table 19) Chemical composition of effusive and dyke rocks from the ophiolite association of the Yap and Mariana island arcs
    di: Sharas'kin, Anatoly Ya, et al.
    Pubblicazione: (1980)
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