| 花岗岩的形成及构造环境——试论陆壳岩石圈岩浆孕育带 |
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| 引用本文： | 郭华春. 花岗岩的形成及构造环境——试论陆壳岩石圈岩浆孕育带[J]. 岩土工程界, 1997, 0(6) |
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| 作者姓名： | 郭华春 |
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| 作者单位： | 有色总公司新疆地勘局物探大队 |
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| 摘 要： | 大陆板块在碰撞时，岩石圈中形成以拆离面为主体的构造通道和减压区，特殊地段形成热能和热流体的聚集区，并逐渐发展成岩浆孕育带。建立了三个常见的岩浆孕育带模型。强调花岗岩主要形成于陆壳中上层。
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| 关 键 词： | 花岗岩 构造 岩浆孕育带 |
DIAGENESIS OF GRANITE AND TECTONIC SETTING:ON MAGMATIC BREEDING BELT OF CONTINENTAL LITHOSPHERE |
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| Guo Huachun. DIAGENESIS OF GRANITE AND TECTONIC SETTING:ON MAGMATIC BREEDING BELT OF CONTINENTAL LITHOSPHERE[J]. Geotechnical Engineering World, 1997, 0(6) |
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| Authors: | Guo Huachun |
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| Abstract: | The structural conduct and depressure area, congregation area for heat energy and thermal fluid, was formed in lithosphere in the process of continental plate collision, and gradually developed into magmatic breeding belt. The three common magmatic breeding models were established. It was stressed that granite is mainly formed in the middle and upper level of continental crust. |
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| Keywords: | granite structure breeding zone of magma |
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