在如此宽广的岩浆岩床烘烤下的有机沉淀物大大增加了甲烷和含碳气体的释放。
That vastly increases the volume of sediments the hot rock can cook and from which methane and other carbon-rich gases can be released.
煌斑岩岩浆晚期残余气液与成矿流体组成相近、沉淀次序相同， 表明它们可能有成因联系。
The last remain fluid of lamprophyre magma is similar to metallogenetic fluid in composition and precipitating sequence, showing their genetic relationship.
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