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豫西东秦岭造山带低压变质带的变质变形和变质反应
引用本文:周汉文,陈能松.豫西东秦岭造山带低压变质带的变质变形和变质反应[J].地球科学,1994,19(1):9-18.
作者姓名:周汉文  陈能松
作者单位:中国地质大学地质系 武汉430074
基金项目:国家自然科学基金(48900015)资助项目
摘    要:豫西西峡北部低压变质带受到4次变形改造。低压变质作用主要发生在D1和D2变形间期,形成黑云母-红柱石、石榴石-红柱石、十字石-红柱石和堇青石-红柱石4个递增变质带。由矿物变质反应识别出堇青石-红柱石带p-T趋势具有减压增温特点,这一演化特征可能反映变质作用具有地壳拉张的地球动力学特点。

关 键 词:低压  变质作用  变质反应  秦岭  矿物

Metamorphism, Deformation and Metamorphic Reactions of Low-Pressure Metamorphic Belt in East Qiriling Orogenic Belt, Western Henan
Zhou Hanwen,Chen Nengsong.Metamorphism, Deformation and Metamorphic Reactions of Low-Pressure Metamorphic Belt in East Qiriling Orogenic Belt, Western Henan[J].Earth Science-Journal of China University of Geosciences,1994,19(1):9-18.
Authors:Zhou Hanwen  Chen Nengsong
Abstract:Low-pressure metamorphic belt (LPB)in northern Xixia of Western Henan were affected by four major deformation events. The low-pressure metamorphism took place mainly during the intermittence of D, and D2 deformation phases, forming four prograde metamorphic zones:biotite-andalusite zone, garnet-andalusite zone, staurolite-andalusite zone and cordierite-andalusite zone. The p-T trajectory constrained by mineral metamorphic reaction in cordierite-andalusite zone is characterized by increas-ing in temperature and decreasing in pressure. which reflects the crust extension geodynamics during metamorphism.
Keywords:low-pressure metamorphism  relationship between metamorphism and deformation  metamorphic reaction  p-T trajectory  crust extension  Qinling  Western Henan  
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