江苏连云港江宁工业园区块地热地质特征与地热远景评价研究  

Geothermal Geological Characteristics and Geothermal Prospective Evaluation of Jiangning Industrial Park in Lianyungang,Jiangsu

作　　者：王陆超[1] WANG Luchao(The Sixth Geological Brigadeof Jiangsu Geological and Mining Bureau,Lianyungang,Jiangsu 222023,China)

机构地区：[1]江苏省地质矿产局第六地质大队,江苏连云港222023

出　　处：《中国锰业》2018年第5期101-104,共4页China Manganese Industry

摘　　要：研究区大地构造位置属于秦岭大别造山带东延的大别—苏鲁造山带的苏鲁高压—超高压变质带的连云港—泗阳断块内,区内构造早期以韧性剪切变形构造发育为特征,晚期则以脆性断裂构造为主。研究区地质构造复杂,具备较好的地热地质条件,地热资源属于对流型地热。在对研究区地热地质特征进行分析的基础上,进而深入对地热资源进行评价研究,对研究区以后的工作具有十分重要的指导作用。The geotectonic position in the study area belongs to Lianyungang Siyang fault block of Su Lu high pressure metamorphic belt of Dabie Sulu orogenic belt, including the Dabieorogenic belt of the Dabieorogenic belt and Qinling Mountains. The early structural development of the area is characterized by ductile shear deformation structure. In the late stage, it is mainly brittle fracture. The geological structure of the study area is complex and it has better geothermal geological conditions. Geothermal resources are of convective and geothermal resources. On the basis of the analysis of geothermal geological characteristics in the study area, this paper further evaluates geothermal resources and it has a very important guiding role for the future work of the study area.

关 键 词：地热地质特征 地热远景 江宁工业园区块 

分 类 号：P314[天文地球—固体地球物理学]