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大别山东麓前寒武纪二长花岗质片麻岩抬升冷却过程的递进变形
引用本文:张家声,江来利,许建东.大别山东麓前寒武纪二长花岗质片麻岩抬升冷却过程的递进变形[J].地质科学,2003,38(1):114-127.
作者姓名:张家声  江来利  许建东
作者单位:1. 中国地震局地质研究所, 北京, 100029;2. 安徽省地质调查院, 合肥, 230001
基金项目:由国家重点基础研究发展规划 (G1 9990 75 5 1 1 ),国家自然科学基金 ( 40 1 72 0 77)资助。
摘    要:大别山东麓北段结晶基底中的二长花岗质岩石具长石应力支撑结构,早期高级变质作用条件下的韧性推覆以长石类矿物普遍晶质塑性变形和同构造重结晶作用为典型特征,晚期在发育糜棱岩的低级韧性剪切变形阶段处于脆性状态,在其内部和边缘形成了包括微角砾岩、假玄武玻璃、黑色超糜棱岩和熔结超碎裂岩等脆性断层岩石.二长花岗质岩石中不同类型韧性和脆性断层岩石的成因和构造联系,记录了大别地体的抬升冷却历史和不同阶段构造变动的性质.

关 键 词:递进变形  抬升冷却  糜棱片麻岩和糜棱岩  微角砾岩  大别山东麓
收稿时间:2002-04-29
修稿时间:2002年4月29日

PROGRESSIVE DEFORMATION OF PRECAMBRIAN ADAMELLITIC GNEISSES RESPONSE TO AN UPLIFT-RELATED COLLING IN EASTERN DABIE MOUNTAINS, CENTRAL CHINA
Zhang Jiasheng,Jiang Laili,Xu Jiandong.PROGRESSIVE DEFORMATION OF PRECAMBRIAN ADAMELLITIC GNEISSES RESPONSE TO AN UPLIFT-RELATED COLLING IN EASTERN DABIE MOUNTAINS, CENTRAL CHINA[J].Chinese Journal of Geology,2003,38(1):114-127.
Authors:Zhang Jiasheng  Jiang Laili  Xu Jiandong
Institution:1. Institute of Geology, China Seismological Bureau, Beijing 100029;2. Geological Survey of Anhui Province, Hefei 230001
Abstract:The adamellitic gneisses in the basement in northern segment of eastern Dabie Mountains were characterized by feldspars stress-suppporting framework in response with deformation. All feldspars in the rocks involved into an earlier high-grade ductile thrusting were sheared by crystal plasticity mechanism. The adamellitic gneisses were in brittle state during a late low-grade ductile shearing when various brittle fault rocks, including micro breccia, pseudotachylyte, black ultramylonite and sintered cataclasite, were formed within or on the rim of the adamellitic gneisses. Origin of the various ductile to brittle deformation rocks and their structural relationships recorded an uplift-related cooling history of the Dabie terrain and the deformation process in different stages.
Keywords:Progressive deformation    Uplift-related cooling    Mylonitic gneiss and mylonites    Microbreccia    Eastern Dabie Mountains
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