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江西萍乐凹陷构造-沉积演化的基本特征及对找煤预测的启示
引用本文:许德如,王力,王智琳,吴俊,吴传军.江西萍乐凹陷构造-沉积演化的基本特征及对找煤预测的启示[J].大地构造与成矿学,2011,35(4):513-524.
作者姓名:许德如  王力  王智琳  吴俊  吴传军
作者单位:1. 中国科学院广州地球化学研究所矿物学与成矿学重点实验室,广东广州,510640
2. 中国科学院广州地球化学研究所矿物学与成矿学重点实验室,广东广州510640;中国科学院研究生院,北京100049
3. 中国科学院广州地球化学研究所矿物学与成矿学重点实验室,广东广州510640;中国科技大学地球和空间科学学院,安徽合肥230026
基金项目:全国危机矿山接替资源找矿项目(项目编码200736030)资助
摘    要:中新生代以来,江西萍乐(萍乡-乐平)凹陷带的构造-沉积演化经历了三期四个阶段,即:印支期大规模的推覆、燕山早期晚三叠世末的基底拆离和褶皱-逆冲以及早侏罗世末的盖层滑脱、喜山期新近纪盖层和基底的滑覆,反映盆地性质具有断(裂)陷与坳陷的多次转换特征.构造运动对煤层的控制也表现为坳陷导致煤系地层盖层加厚、埋藏加深及错断、重复...

关 键 词:萍乐凹陷  构造演化  推覆构造  找煤预测

Tectonic-Sedimentary Characteristics of the Ping(Pingxiang)-Le(Leping) Depression in Jiangxi Province and its Implications on Coal Mineral Resource Prospecting
XU Deru,WANG Li,WANG Zhilin,WU Jun,WU Chuanjun.Tectonic-Sedimentary Characteristics of the Ping(Pingxiang)-Le(Leping) Depression in Jiangxi Province and its Implications on Coal Mineral Resource Prospecting[J].Geotectonica et Metallogenia,2011,35(4):513-524.
Authors:XU Deru  WANG Li  WANG Zhilin  WU Jun  WU Chuanjun
Institution:XU Deru1,WANG Li1,2,WANG Zhilin1,WU Jun1,2 and WU Chuanjun1,3(1.CAS Key Laboratory of Mineralogy and Metallogeny,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,Guangdong,China,2.Graduate School of Chinese Academy of Sciences,Beijing 100049,3.School of Earth and Space Sciences,University of Science and Technology of China,Hefei 230026,Anhui,China)
Abstract:The formation of the Ping(Pingxiang)-Le(Leping) coal-bearing depression zone was strictly controlled by three-period and four-stages of tectonic-sedimentary evolution from Mesozoic to Cenozoic.These include Nappe-stage in Indosinian,basal-detachment and fold-thrust stage in the end of the Late Triassic and cover strike-slip stage in the end of the Early Jurassic,and cover and basal sliding stage during Himalayan.Thus,multistage conversion between sag and fault depression made the basin type of the Pingle de...
Keywords:Pingle depression  tectonic-sedimentary evolution  nappe structure  coal mine predicting  
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