Hydrocarbon gases and fluid evolution in very low-grade metamorphic terranes: A case study from the Central Swiss Alps

被引：0

作者：

Mazurek, M ^{[1
]}

Waber, HN ^{[1
]}

Gautschi, A ^{[1
]}

机构：

[1] Univ Bern, Inst Geol & Mineral, GGWW, Bern, Switzerland

来源：

WATER-ROCK INTERACTION | 1998年

关键词：

D O I：

暂无

中图分类号：

X [环境科学、安全科学];

学科分类号：

08 ; 0830 ;

摘要：

In a marl formation that was subjected to low-temperature metamorphism, free gases and groundwaters were sampled and compared with the bulk and isotopic compositions of fluid inclusions. Results indicate different sources for gas (derived thermally from kerogen) and water (which represents a mixture of connate and metamorphic water). No indications exist for later interactions of the rocks with meteoric waters.

引用

页码：417 / 420

页数：4

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