Geothermal measurements in the pilot-boreholes of the china continental scientific drilling |
| |
Authors: | Wang Jiyang Hu Shengbiao Yang Wencai Chen Benhe Chen Zhenyan Li Tiejun |
| |
Affiliation: | (1) Institute of Geology and Geophysics, Chinese Academy of Sciences, 100029 Beijing, China;(2) Institute of Geology, Ministry of Land and Resources of China, 100037 Beijing, China |
| |
Abstract: | The geothermal measurements in the pilot boreholes of the China Continental Scientific Drilling (CCSD) indicate that the temperature
gradients in the target area of the deep drilling range from 19 to 26°C/km, which is lower than that (25–0°C/km) for the global
continental area and similar to that for the KTB (21–28°C/km). Ther mal conductivity measurements for 44 core samples show
that the ultra-high pressure (UHP) metamorphic rocks have 50% higher thermal conductivity (with a mean of 3.94±1.26 W/mK)
than that for the average value of the upper crust. The measured heat flow values vary between 76 and 80 mW/m2, higher than that for the global continental area (65±1.6 mW/m2) and the continental China (61±15.5 mW/m2) as well as the adjacent North Jiangsu Basin (68 mW/m2), but lower than that below 1000 m in the KTB (85 mW/m2). The elevated heat flow in the pilot-boreholes can be attributed to the lateral heat concentration due to higher rock thermal
conductivity of the UHP belt than that of the adjacent rocks. Lower deep temperature in the target area of the deep drill
ing can be expected due to the lower measured temperature gradient, which means that the Sulu area is geothermally suitable
for continental deep drilling. |
| |
Keywords: | temperature gradient thermal conductivity heat flow CCSD North Jiangsu |
本文献已被 SpringerLink 等数据库收录! |
| 点击此处可从《中国科学通报(英文版)》浏览原始摘要信息 |
|
点击此处可从《中国科学通报(英文版)》下载全文 |