江西省萍乡市源泣隐伏煤田区地质特征及找矿方向浅析  

The Geological Characteristics and Exploration Direction In Yuanban Concealed Coalfield in Pingxiang City, Jiangxi Province

作　　者：兰万国 王森林[1] 

机构地区：[1]江西省地质矿产勘查开发局九0一地质大队,江西萍乡337000

出　　处：《中国科技纵横》2010年第22期215-215,271,共2页China Science & Technology Overview

摘　　要：源澈地区所见的老地层不是“古隆起”，而是由多个滑覆体依次堆叠的滑覆构造形成的外来岩系，这些外来岩系之下，隐伏着大片的安源煤系。同时，源澎地区的主要含煤地层为上三叠纪安源群紫家冲组（T3a），属萍乡市开采的主要煤层。因此，源溢地区是一个理想的寻找隐伏煤田的地区。Old formation in Yuanban area is not ＂ancient uplift＂, but exotic rock. The exotic rock is composed of sliding tectonics, which is become from the stack of multiple sliding bodies. Large coal formation is concealed under these exotic rocks. At the same time, T3a is the main coal-bearing strata in Yuanban area, which belong to the main mining coal in pingxiang. Therefore, Yuanban area is an ideal place for concealed coalfield.

关 键 词：隐伏煤田 地质特征 找矿方向 萍乡市 

分 类 号：P618.110.8[天文地球—矿床学]