O-18-ENRICHMENT OF SILICIC MAGMAS CAUSED BY CRYSTAL FRACTIONATION AT THE GALAPAGOS SPREADING CENTER

被引：83

作者：

MUEHLENBACHS, K

BYERLY, G

机构：

[1] UNIV ALBERTA,DEPT GEOL,EDMONTON T6G 2E3,ALBERTA,CANADA

[2] LOUISIANA STATE UNIV,DEPT GEOL,BATON ROUGE,LA 70803

来源：

CONTRIBUTIONS TO MINERALOGY AND PETROLOGY | 1982年 / 79卷 / 01期

关键词：

D O I：

10.1007/BF00376963

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

引用

页码：76 / 79

页数：4

共 37 条

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[5] MINOR AND TRACE-ELEMENT GEOCHEMISTRY OF VOLCANIC-ROCKS DREDGED FROM THE GALAPAGOS SPREADING CENTER - ROLE OF CRYSTAL FRACTIONATION AND MANTLE HETEROGENEITY
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[J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2021, 22 (11)
[7] DIRECT EVIDENCE FOR THE ORIGIN OF LOW-O-18 SILICIC MAGMAS - QUENCHED SAMPLES OF A MAGMA CHAMBERS PARTIALLY-FUSED GRANITOID WALLS, CRATER LAKE, OREGON
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[J]. EARTH AND PLANETARY SCIENCE LETTERS, 1989, 96 (1-2) : 199 - 208
[8] Rapid generation of both high- and low-δ18O, large-volume silicic magmas at the Timber Mountain/Oasis Valley caldera complex, Nevada
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Valley, JW
[J]. GEOLOGICAL SOCIETY OF AMERICA BULLETIN, 2003, 115 (05) : 581 - 595
[9] Tectonic and climate history influence the geochemistry of large-volume silicic magmas: New δ18O data from the Central Andes with comparison to N America and Kamchatka
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de Silva, Shanaka L.
Bindeman, Ilya N.
Cas, Raymond A. F.
[J]. JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, 2013, 262 : 90 - 103
[10] DETERMINATION OF PRE-ERUPTIVE H2O, F AND CL CONTENTS OF SILICIC MAGMAS USING MELT INCLUSIONS - EXAMPLES FROM TAUPO VOLCANIC CENTER, NEW-ZEALAND
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