ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
贵德盆地热结构及地热成因机制
  
关键词:Guide basin  geothermal fluid  thermal storage temperature  genetic mechanism  thermal structure of the earth's crust
基金项目:中国地质调查项目“贵德盆地深部水文地质调查”(编号: 12120114024701); 国家青年科学基金“盆地岩石圈热结构的精确识别与模型验证——以青海贵德盆地为例”(编号: 41402231)
作者单位E-mail
郎旭娟 中国地质科学院水文地质环境地质研究所
中国地质科学院岩溶地质研究所 
langlan77@163.com 
张发旺 中国地质科学院岩溶地质研究所 guilingw@163.com 
王贵玲 中国地质科学院水文地质环境地质研究所  
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摘要:
The Thermal Structure and Geothermal Genesis Mechanism in Guide Basin
      Guide basin belongs to Cenozoic period fault ba-sin, which is surrounded by hills that located in the Yellow River valley, northeastern margin of the Ti-betan Plateau; from the perspective of geomorphicu-nits it is located the QingHai–Tibet block, which among the Qilian–Kunlun–Qinlingorogenic belts. The study area have a series of faults in the NWW, NW and NNW direction, the intense neotectonic activity provides good geothermal geological conditions for high temperature geothermal system. There are vari-ous types of geothermal manifestation in study area, and have intense hydrothermal activities, especially in the west of the basin - Zhacangsi thermal field, where the water temperature is as high as 93℃. However, limitedby the objective conditions, the development and utilization of geothermal resources in the area and the related research are not yet perfect:
LANG Xu-juan,ZHANG Fa-wang,WANG Gui-ling.2017.The Thermal Structure and Geothermal Genesis Mechanism in Guide Basin[J].Acta Geoscientica Sinica,38(s1):43-46.
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