晋南晚中生代古地热场特征及其热源探讨  

CHARACTERISTICS AND MECHANISM OF LATE MESOZOIC PALEO-GEOTHERMOL FIELD IN SOUTHERN SHANXI

作　　者：宋党育[1] 秦勇[1] 

机构地区：[1]中国矿业大学资源与环境学院,徐州221008

出　　处：《中国煤田地质》1998年第4期32-34,共3页Coal Geology of China

基　　金：国家自然科学基金(编号:49472125)部分研究内容

摘　　要：应用煤系脉体流体包裹体分析以及 EASY%Ro 数值模拟方法,研究了山西南部晚古生代煤的煤化作用古地热场特征,得出本区晚中生代具有异常高热古地热场的结论,进而探讨了异常古地热场的形成机制。Bsaed upon the methods of the fluid inchusion analysis and EASY% R_o numerical simulation,the Late Mesozoic paleo-geothermal field in southern Shanxi was studied,the conclusion that there existed a abnormal paleo-geothermal field in the area was suggested,and mechanism under which the abnormal field was formed was further discussed.

关 键 词：晚中生代 古地热场 数值模拟 热源 

分 类 号：P314.2[天文地球—固体地球物理学]