Formation of granitoids of Caucasus Mineral Waters: Evidence from study of melt and fluid inclusions in minerals

被引：1

作者：

Kurchavov, A. M. ^{[1
]}

Tolmacheva, E. V. ^{[2
]}

Bogatikov, O. A. ^{[1
]}

Kotov, A. B. ^{[2
]}

机构：

[1] Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow, Russia

[2] Russian Acad Sci, Inst Precambrian Geol & Geochronol, St Petersburg, Russia

来源：

DOKLADY EARTH SCIENCES | 2013年 / 452卷 / 01期

基金：

俄罗斯基础研究基金会;

关键词：

Fluid Inclusion; DOKLADY Earth Science; Titanite; Dark Band; Magma Intrusion;

D O I：

10.1134/S1028334X13090171

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

[No abstract available]

引用

页码：958 / 962

页数：5

共 7 条

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[2]

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[3]

Kurchavov A. M., 2009, MAGMATISM ORE FORMAT, P75

[4] Heterogeneity of Ar and Sr initial isotopic composition in the coexisting minerals from Miocene hypabyssal granitoids in the Caucasian Mineral Waters region [J].

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Avdeenko, A. S. ;

Nosova, A. A. ;

Dokuchaev, A. Ya. ;

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Gol'tsman, Yu. V. .

DOKLADY EARTH SCIENCES, 2006, 410 (07) :1070-1074

[5]

Nosova AA, 2005, PETROLOGY+, V13, P122

[6]

ROEDDER E, 1984, REV MINERAL, V12, P1

[7]

Sobolev N. D., 1959, NEOGENE INTRUSIONS P

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