西昆仑地震展布与塔西南“A”型俯冲

1997年 19卷 第1期
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SEISMIC SPREAD IN WEST KUNLUN AND A-TYPE SUBDUCTION IN SOUTHWEST TARIM
吴世敏 马瑞士 卢华复 贾承造
Wu Shimin Ma Ruishi Lu Huafu Jia Chengzao
南京大学地球科学系, 210093 2. 塔里木石油勘探指挥部地质研究中心, 新疆库尔勒 841000
Departmeat of Earth Sciences, Nanjing University 2. Research Ceater of Geology, Tarim Headquarters of Petroleum Exploration
通过对西昆仑地震展布、新生代火山岩及塔西南转换波测深、晚期第三纪以来沉积等特征的分析研究,表明塔里木大陆岩石圈正往西南即西昆仑之下进行“A”型俯冲作用。最后,作者对“A”型俯冲的形成机理进行了探讨。
By studing seismic spread and Cenozoic igneous rocks in West Kunlun, the detection of converted waves and deposit since the Late Quaternary in Southwest Tarim and other characteristics, it is revealed that Tarim continent lithosphere is subducting southwestward beneath West Kunlun in A-type subduction. At last, the forming mechanism of A-type subduction is discussed.
西昆仑; 地震; 火山岩; “A”型俯冲;
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https://doi.org/10.11781/sysydz199701001