焦作——济源地区晚中生代古地热场特征及成因  

CHARACTERISTICS AND MECHANISM OF THE LATE MESOZOIC PALAEOGEOTHERMAL FIELD IN JIAOZUO—JIYUAN,HENAN,CHINA

作　　者：秦勇[1] 金法礼[1] 权彪[1] 曹作华[1] 李大华 

机构地区：[1]中国矿业大学,徐州221008 [2]四川煤田地质研究所,重庆630037

出　　处：《煤田地质与勘探》1993年第3期16-23,T001,共9页Coal Geology & Exploration

摘　　要：用各种地质温度计和地质压力计确定了研究区晚中生代古地热场的基本特征,并由此得出了该古地热场具有异常、瞬时两大特点的初步结论。进而讨论了异常地热场的形成机理。The fundamental characteristics of the Late Mesozoic palaeogeothermal field in Jiaozuo-JiyuanWere studied in line with some geothermal and geopressured indicators.And it was concluded that there existedthe abnormal and transient peculiarities in the field.Basing upon the results,the mechanism on the formation ofthe abnormal geothermal field was further gone into in combine with the relative geological data.

关 键 词：古地热场 形成机理 晚中生代 地热 

分 类 号：P314.2[天文地球—固体地球物理学]