云和盆地早白垩世双峰式火山岩特征 |
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引用本文: | 杨晓春.云和盆地早白垩世双峰式火山岩特征[J].浙江国土资源,1996(2). |
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作者姓名: | 杨晓春 |
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作者单位: | 浙江省第七地质大队!丽水,323000 |
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摘 要: | 本文从岩石学、岩石化学、微量元素及稀土元素等方面,对云和盆地早白垩世馆头组火山岩特征进行了论述,并对其形成环境及成因作了探讨.认为该套火山岩由基性岩及酸性岩构成,缺少SiO2含量在53.17%~68.57%的中性岩,是一套典型的双峰式火山岩组合。指出盆地内火山岩为拉张构造背景下形成,其基性岩和酸性岩具有不同源区,前者源于部分上地幔融熔物质(受陆壳物质混染);后者来自部分地壳融熔的产物。
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关 键 词: | 双峰式火山岩 基性岩 酸性岩 早白垩世馆头组 云和盆地 |
FEATURES OF LOWER CRETACEOUS BIMIDAL VOLCANIC ROCKS IN ZHEJIANG YUNHE BASIN |
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Authors: | Yang Xiaochun |
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Abstract: | The volcanic rocks of lower cretaceous Guantou formation in south-west Zhejiang consist ofbasic rocks and acid rocks, without neutral rocks, of which silica are between 53. 17% and 68.57%. It is a set of. typical bimedal volcanic rock assemblage. On the basin of petrology, Petrc-chemistry, microelement and rare earth element, this paper expounded the features of the volcanic rocks, and discussed its forming environment and genesis. |
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Keywords: | bimodal volcanic rock basic rock acid rock Guantou formaytion Yunhe basin |
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