新疆石油地质 ›› 2001, Vol. 22 ›› Issue (6): 472-474.

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羌塘地区壳内低阻层特征及初步认识

王宜昌1, 王永涛2   

  1. 1.中国石油勘探开发科学研究院遥感所,北京 100083;
    2.石油物探局,河北涿州 072700
  • 收稿日期:2001-07-20 出版日期:2001-12-01 发布日期:2020-10-30
  • 作者简介:王宜昌(1938-),男,高级工程师,地球物理勘探。

Characteristics and Preliminary Knowledge of Inner-Crustal Low Resistivity Zone in Qiangtang Area

WANG Yi-chang, WANG Yong-tao   

  • Received:2001-07-20 Online:2001-12-01 Published:2020-10-30
  • About author:WANG Yi-chang(1938-), Male, Senior Engineer, Geophysical Prospecting, Research Institute of Petroleum Exploration and Development, CNPC, Beijing 100083, China

摘要: 在羌塘地区深达 100 km的大地电磁测深MT)大剖面上,壳内低电阻层显示出不同面貌。南段以“△”块状体为特征;北段低阻层从-100km深处上升至近地表-10 km处,呈巨大的蘑茹体。在平面等值线图上,北羌塘地区以大面积坳隆、东西分块为特征;南羌塘地区以条带状坳隆南北分带为主。研究结果认为,低电阻层与地形相关,这不仅旁证了有关低阻层解释的可靠性,同时说明北羌塘独特的块状高山区地貌是活跃的深部构造运动的表现。研究区地壳既非全是冷壳、也非全是热壳,应是冷壳、热壳呈楔块状相间,尤其是确旦错一带可能存在热柱。这对油气富集、形成、二次成因将有较大的影响。

关键词: 羌塘地区, 地壳, 低电阻, 地层

Abstract: The inner-crustal low resistivity zones over the profile of crustal magneto-electrotelluric survey beneath 100 km in Qiangtang area show district images which are characterized by massive body symbolided as“△”in southern segment and tremendous mushroom body in northern segment ranging from-100 km up to-10 km in depth. From the view of plane contour diagram, the northern Qiangtang area is characterized by large area of depression-uplift and bulking in its east and west parts, while the southern Qiangtang area by strip depression-uplift and zoning in its south and north parts. The results show that the low resistivity zone is related closely to the landscapes, not only indicating reliability about the zone interpretation,but that the distinctive features like block high mountain range are expressions of active deep tectonic movements. The crustal bodies in studied area are neither cold nor thermal, but cold crust alternates with thermal crust in form of wedge,,along the Quedancuo area may exist thermal plume,all of which has greater effect on its petroleum accumulation, generation and secondary origin.

Key words: Qiangtang area, crust, Low resistivity, formation

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