| 准噶尔盆地热流及地温场特征 |
| |
| 引用本文： | 王社教,胡圣标,汪集旸. 准噶尔盆地热流及地温场特征[J]. 地球物理学报, 2000, 43(6): 771-779 |
| |
| 作者姓名： | 王社教 胡圣标 汪集旸 |
| |
| 作者单位： | 1. 中国科学院地质与地球物理研究所,北京100029;2. 中国石油勘探开发研究院 北京100083;3. 中国科学院地质与地球物理研究所,北京100029 |
| |
| 基金项目： | 中国石油天然气集团公司资助项目，970211-02， |
| |
| 摘 要： | 利用准噶尔盆地 1 96口井的温度资料及 90块岩石样品热导率的测定 ,计算了 35个大地热流数据 ,编制了盆地不同深度现今地温等值线图 .研究结果表明 ,准噶尔盆地现今为低地温、低大地热流的冷盆 ,盆地的现今地温梯度平均为 2 1 2℃ /km ,大地热流密度平均为42 3mW/m2 .热流的分布表现为隆起高、坳陷低的特征 .影响地温场的主要因素包括盆地的深部结构、盆地演化、盆地基底构造形态、地下水活动和沉积层的放射性生热等 .
|
| 关 键 词： | 准噶尔盆地 地温场 地温梯度 热导率 大地热流 |
| 收稿时间： | 2000-02-22 |
THE CHARACTERISTICS OF HEAT FLOW AND GEOTHERMAL FIELDS IN JUNGGAR BASIN |
| |
| WANG SHE-JIAO,HU SHENG-BIAO,WANG JI-YANG. THE CHARACTERISTICS OF HEAT FLOW AND GEOTHERMAL FIELDS IN JUNGGAR BASIN[J]. Chinese Journal of Geophysics, 2000, 43(6): 771-779 |
| |
| Authors: | WANG SHE-JIAO HU SHENG-BIAO WANG JI-YANG |
| |
| Affiliation: | 1. Institute of Geology and Geophysics , Chinese Academy of Sciences, Beijing 100029, China ;2. Research Institute of Petroleum Exploration and Development , Beijing 100083, China |
| |
| Abstract: | Based on the temperature data of 196 wells and measurements of 90 thermal conductivity of rocks in Junggar Basin, 35 terrestrial heat flow values are caculated. The results show that the Junggar Basin is a relatively “cold basin” now, with lower temperature and lower heat flow. Mean values of temperature gradient and heat flow are about 21.2℃/km and 42.3mW/m 2, respectively. Higher heat flow in the uplift and lower in the depression are observed. The distribution of heat flow and temperature is affected by hydrothermal circulation, structure of basement and evolution of the Junggar basin, as well as radioactive heat production in sedimentary rocks. [ |
| |
| Keywords: | Junggar basin Geothermal field Temperature gradient Thermal conductivity Heat flow |
| 本文献已被 维普 万方数据 等数据库收录！ |
| 点击此处可从《地球物理学报》浏览原始摘要信息 |
|
点击此处可从《地球物理学报》下载全文 |
|
