HEAT FLOW MEASUREMENTS IN PANZHIHUA-XICHANG(PANXI) PALEORIFT ZONE, SW CHINA

作     者：汪集暘 汪缉安 黄少鹏 张文仁 周友松 金昕 

作者机构：Institute of Geology Academia Sinica Beijing Geophysical Brigade Panxi Geological Team of Sichuan Geological Bureau Xichang Geophysical Brigade Panxi Geological Team of Sichuan Geological Bureau Xichangeat flow measurements are of great significance in rift studies. The Panxi area has. been considered to be a paleorift zone of the Hercynian-Indosinian period. For a long time the geological and geophysical community are greatly concerned about the thermal state and the possibility of the existence of high heat flow in this region. And great efforts and research work have been made by joint geothermal study program of Geother 

出 版 物：《Chinese Science Bulletin》 (科学通报(英文版))

年 卷 期：1987年第32卷第8期

页      面：550-554页

学科分类：0709[理学-地质学] 081803[工学-地质工程] 07[理学] 08[工学] 0818[工学-地质资源与地质工程] 

主　　题：concerned geophysical possibility strata PALEORIFT ZONE PANXI SW CHINA mudstone Paleozoic rock 

摘      要：Heat flow measurements are of great significance in rift studies. The Panxi area has. been considered to be a paleorift zone of the Hercynian-Indosinian period. For a long time, the geological and geophysical community are greatly concerned about the thermal state and the possibility of the existence of high heat flow in this region. And great efforts and research work have been made by joint geothermal study program of