王一波^1,2,3,,
胡圣标^1,2,3,,,
聂栋刚⁴,
张克松⁴,
姜光政^1,2,
王朱亭^1,2,3
1. 中国科学院地质与地球物理研究所岩石圈演化国家重点实验室, 北京 100029
2. 中国科学院大学地球与行星科学学院, 北京 100049
3. 中国科学院地球科学研究院, 北京 100029
4. 安徽省地勘局第一水文工程地质勘查院, 安徽蚌埠 233000

基金项目: 安徽省基金项目"安徽省大地热流基础测量"（2014-g-11），江苏省基金项目"苏北盆地地温场调查及地壳热结构专题研究（JITC-1802AW2292）"和国家科技重大专项（2017ZX05008-004）联合资助


详细信息

作者简介: 王一波, 男, 1993年生, 构造地质学专业博士生, 主要研究方向:大地热流, 流变结构和动力学机制.E-mail:ybwang@mail.iggcas.ac.cn

通讯作者: 胡圣标, 男, 1963年生, 研究员, 毕业于中国科学院地质与地球物理研究所, 主要从事地热学研究.E-mail:sbhu@mail.iggcas.ac.cn

中图分类号: P314

收稿日期:2019-01-22
修回日期:2019-06-23
上线日期:2019-08-05

Is the Tan-Lu fault zone a thermal anomaly belt:Constraints from heat flow in its southern section

WANG YiBo^1,2,3,,
HU ShengBiao^1,2,3,,,
NIE DongGang⁴,
ZHANG KeSong⁴,
JIANG GuangZheng^1,2,
WANG ZhuTing^1,2,3
1. Institute of Geology and Geophysics Chinese Academy of Sciences, State Key Laboratory of Lithospheric Evolution, Beijing 100029, China
2. University of Chinese Academy of Sciences, College of Earth and Planetary Sciences, Beijing 100049, China
3. Chinese Academy of Sciences, Institutions of Earth Science, Beijing 100029, China
4. Institute of Anhui Bureau of Geological Exploration, First Hydrology and Engineering Geological Exploration, Bengbu Anhui 233000, China


More Information

Corresponding author: HU ShengBiao,E-mail:sbhu@mail.iggcas.ac.cn

MSC: P314

--> Received Date: 22 January 2019
Revised Date: 23 June 2019
Available Online: 05 August 2019


摘要
摘要:郯庐断裂带是东亚最重要的断裂之一，在构造地质、岩石矿物、地震分布等领域得到了广泛的关注，然而少有针对郯庐断裂带地热学的研究.本文作者对郯庐断裂带南段7口钻井进行了系统测温，采用光学扫描法测试了6口钻井的142块岩心和13块露头样品的热导率，获得了6个高质量的热流数据.结合已发表的热流和地震剖面资料，我们获得了郯庐断裂带南段的岩石圈结构.研究表明，郯庐断裂带南段现今地温梯度从南到北有增大的趋势，介于21.8~30.3℃·km^-1.大地热流值介于44.0~81.7 mW·m^-2，平均61.4±10.8 mW·m^-2，表现为正常大地热流的特征，并非热异常带.最大热流值出现在庐枞盆地的大陆科学钻探井ZK03处，上地壳浅部极高的生热层很可能是高热流的主要因素.沿郯庐断裂南段地震带浅源地震发震带的底界和350℃等温面耦合较好，指示了深部结构的差异.
关键词: 热导率/
热流/
震源深度/
生热率/
热结构/
郯庐断裂带

Abstract:The Tan-Lu fault zone is one of the most important faults in East Asia. It has received extensive attention of many fields such as structural geology, mineralogy, and seismology. However, few geothermal studies on this structure have been made so far. This work conducted temperature measurement on 7 wells systematically in the southern Tan-Lu fault zone. Thermal conductivity of 142 cores and 13 outcrop samples for these wells were tested by the optical scanning method and 6 high-quality heat flow data were obtained. Combined with the published heat flow and seismic profiles, we obtained the lithospheric structure of the southern Tan-Lu fault zone. The study shows that the current temperature gradient in the study area increases from south to north, ranging from 21.8 to 30.3℃·km^-1. The heat flow value is between 44.0~81.7 mW·m^-2, with an average of 61.4±10.8 mW·m^-2, represnting a normal geothermal heat flow rather than a thermal anomaly belt. The maximum heat flow value appears in the Continental Scientific Drilling Well ZK03 in the Luzong Basin and the extremely high heat production of rocks in the shallow upper crust is probably the main factor for such a high heat flow. The bottom boundary of the shallow earthquake seismic zone in the southern Tan-Lu fault zone is well coupled with the 350℃ isothermal surface, indicating the difference in deep structure.
Key words:Thermal conductivity/
Heat flow/
Focal depth/
Heat production/
Thermal structure/
Tan-Lu fault zone



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