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东秦岭松树沟长英质高压麻粒岩的原岩性质
引用本文:王焰,刘良.东秦岭松树沟长英质高压麻粒岩的原岩性质[J].西北大学学报,1997,27(6):525-528.
作者姓名:王焰  刘良
作者单位:西北大学地质学系,西北大学地质学系,西北大学地质学系 710069,西安,710069,西安,710069,西安
基金项目:国家自然科学基金资助课题(49672141)
摘    要:地球化学特征研究表明,东秦岭松树沟长英质高压麻粒岩的原岩性质主体为杂砂岩或长石砂岩,少量为亚碱性的酸性火山岩或岩浆岩并具慢源成因;其古构造环境类似于活动大陆边缘。

关 键 词:长英质高压麻粒岩  秦岭杂岩  原岩性质  古构造环境  东秦岭松树沟

Protolith Properties of High-Pressure Quartzo-Feldspathic Granulite Discovered in Songshugou Area, East Qinling
Wang Yan,Liu Liang,Zhou Dingwu.Protolith Properties of High-Pressure Quartzo-Feldspathic Granulite Discovered in Songshugou Area, East Qinling[J].Journal of Northwest University(Natural Science Edition),1997,27(6):525-528.
Authors:Wang Yan  Liu Liang  Zhou Dingwu
Abstract:A study on geochemical character of high-pressure quartzo-feldspathic granulite in Songshugou area, east Qinling, shows that its protolith is composed mainly of graywacke or arkose, and a little of subalkaline acid volcanic rock or magmatic rock with characteristies of mantle source. Its paleotectonic setting is similar to that of active continental margin.
Keywords:high-pressure  quartzo-feldspathic  granulite  Qinling  complex  protolith  property  paletectonic environment  east Qinling Songshugou
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