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西藏定结幅前寒武系结晶基底中发现基性麻粒岩 被引量:2

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出处 《地质科技情报》 CAS CSCD 北大核心 2001年第3期40-46,共2页 Geological Science and Technology Information
基金 国土资源部 1: 2 5万定结幅区域地质调查项目 ( 2 0 0 0 130 0 0 14 5 )
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  • 1沈渭洲,王德滋,谢永林,刘昌实.湖南千里山复式花岗岩体的地球化学特征和物质来源[J].岩石矿物学杂志,1995,14(3):193-202. 被引量:25
  • 2徐启东.国外陆壳岩石缺乏流体熔融实验和模拟的主要成果[J].地球科学进展,1997,12(2):144-151. 被引量:4
  • 3Searle M P,Parrish R R,Hodges K V,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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  • 5Searle M P. Emplacement of Himalayan leucogranites by magma injectin along giant sill complexes :Examples from the Cho Oyu, Gyachung Kang and Everest leucogranites (Nepal Himalaya )[J]. Journal of Asian Earth Sciences, 199 9,17:773-783.
  • 6le Fort P. Himalayas :The collided range present knowledge of the continental arc[J]. Am. J. Sci. , 1975,275 :1-44.
  • 7England P,le Fort P,Molnar P,et al. Heat sources for Tertiary magmatism and anatexis in the Annapurna Manaslu region of Central Nepal[J]. J. Geophys. Res. ,1992,97:2 107-2128.
  • 8Bird P. Initiation of intracontinental subduction in the Himalaya[J]. J. Geophys. Res. , 1978,83 : 4 975 - 4 987.
  • 9Schott B,Schmeling H. Delamination and detachment of a lithospheric root [J]. Tectonophysics, 1988,296 : 225 - 247.
  • 10Visona D, Lombardo B. Two-mica and tourmaline leucogranites from the Everest-Makalu region(Nepal-Tibet). Himalayan leucogrnaites genesis by isobaric heating?[J]. Lithos , 2002,62:125-150.

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