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历时三年的阿尔金活断层研究,于1988年8月4日至23日在野外现场和乌鲁木齐召开总结验收会,国家地震局科技司聘请了活动断层和古地震研究方面的专家丁国瑜、张裕明、汪一鹏、叶洪、侯珍清、朱海之、石鉴邦、高维明、崔中元、冯先岳,对这一课题进行了认真的检查和验收工作。阿尔金断层是亚洲大陆西部一条巨大的走向滑动断层,全长1600km,跨越西藏、新疆、青海和甘肃四省区,是青藏高原北部的自然边界,明显地分隔了塔里木和柴达木这两个内陆盆地,中外学者十分关心和
For three years, the Altun active fault study was held at the field site and Urumqi from August 4 to August 23, 1988. The Science and Technology Department of the State Seismological Bureau hired experts on active faults and paleoearthquakes, including Ding Guoyu and Zhang Yuming Wang Yipeng, Ye Hong, Hou Zhenqing, Zhu Haizhi, Shi Jianbang, Gao Weiming, Cui Zhongyuan and Feng Xiangyue conducted serious inspection and acceptance work on this issue. The Altyn Tagh fault is a giant strike-slip fault in the western part of the Asian continent with a total length of 1,600 km. It stretches across the four provinces of Tibet, Xinjiang, Qinghai and Gansu provinces and is the natural boundary of the northern part of the Qinghai-Tibet Plateau. It clearly separates Tarim and Qaidam Inland basins, Chinese and foreign scholars are very concerned and