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藏南定结淡色花岗岩——基底隆升降压熔融成因的地质证据

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张金阳, 廖群安. 藏南定结淡色花岗岩——基底隆升降压熔融成因的地质证据[J]. 西北地质, 2004, 37(2): 7-12.
引用本文: 张金阳, 廖群安. 藏南定结淡色花岗岩——基底隆升降压熔融成因的地质证据[J]. 西北地质, 2004, 37(2): 7-12.
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ZHANG Jin-yang, LIAO Qun-an. Leucogranites-geological proof of uplifting, decompressing and melting of the basement, Dingjie, South Tibet[J]. Northwestern Geology, 2004, 37(2): 7-12.
Citation: ZHANG Jin-yang, LIAO Qun-an. Leucogranites-geological proof of uplifting, decompressing and melting of the basement, Dingjie, South Tibet[J]. Northwestern Geology, 2004, 37(2): 7-12.
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藏南定结淡色花岗岩——基底隆升降压熔融成因的地质证据

  • 中国地质大学地球科学学院, 湖北 武汉 430074

  • 基金项目: 中国地质调查局1:25万定结幅区域地质调查项目支持。

Leucogranites-geological proof of uplifting, decompressing and melting of the basement, Dingjie, South Tibet

  • Faculty of Earth Science, China University of Geoscience, Wuhan 430074, China

    摘要
  • 西藏南部定结地区高喜马拉雅结晶基底中淡色花岗岩体紧靠藏南拆离断层内部产出,野外地质和岩相学特征显示其为S型、分两期侵入的淡色花岗岩体——早期的黑云母淡色花岗岩和晚期的白云母淡色花岗岩。基底副变质岩中广泛分布淡色花岗岩脉体,在基底副变质岩中的淡色花岗岩脉体中发现紫苏辉石暗色麻粒岩残留体,这表明本区高喜马拉雅淡色花岗岩源岩为基底副变质岩,且基底副变质岩是在基底快速隆升降压的条件下发生缺水熔融生成的淡色花岗岩岩浆。
    Located immediately in the inner Southern Tibet detachment in the Dingjie region,South Tibet, leucog ranites in the High Hima layancry stalline basement are S-type granites and in truded with two different periods,earlier biotite leucog ranites and later muscovite leucog ranites. The leucog ranites veins occurred widesp readly in the parametam orphic rocks,in which the hypersthene mela-granulited istributed.That suggests the source rocks of leucog ranites of the High Himalaya are parametamorphic rocks. For the ba sement was uplifting,pressure relieved and lacked water,source rocks were melting partly and formed the leucog ranite magma.
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    石耀霖,王其允.高喜马拉雅淡色花岗岩形成的热模拟[J]. 地球物理学报,1997,40(5):667.

    M.P.Searle,R.R.Parrish,K.V.Hodges, et al.. Shisha Pangma Leucogranite, South Tibet Himalayan: field Relation, Geochemistry, Age, Origin, and Emplacement[J]. The Journal of Geology,1997,105:295-314.

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出版历程
收稿日期:  2003-06-18
修回日期:  2004-01-17
刊出日期:  2004-06-15

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