“中国地裂运动观”的创建和发展

ESTABLISHMENT AND DEVELOPMENT OF “CHINESE TAPHROGENY OUTLOOK”

罗志立 赵锡奎 刘树根 雍自全

LUO Zhi-li ZHAO Xi-kui LIU Shu-gen YONG Zi-quan

成都理工学院石油系, 四川成都 610059

Department of Petroleum, Chengdu College of Technology, Chengdu, Sichuan 610059, China

自1981年创立“中国三次地裂运动”的观点以来,得到地学界和社会广泛的反响。文中据20年来国内外大量有关信息,从地裂运动的学术观点对中国地质科学理论发展的促进方面、从陆相生油二元论观点形成及实践检验方面、从峨眉地裂运动观点对四川盆地礁块型气藏的预测有效性方面以及地质同行用此观点解释西南富煤带聚集规律和某些金属矿产成矿构造背景等方面,进行归纳和总结,进而阐述中国基础地质科学和相关应用科学发展的3点经验,并展望“中国地裂运动”研究的方向和前景。

The viewpoint "Chinese three times of taphrogeny" has evoked widespread repercussions in geological circles and society since it was founded in 1981. Based on great amount of related information at home and abroad in recent 20 years, the promotion of the academic standpoint of taphrogeny to the development of Chinese geological scientific theories, the formation and practical examination of the dualistic theory of continental oil generation, the effectiveness of the standpoint of Emei taphrogeny to the prediction of reef segment-typed gas pools in the Sichuan Basin, and the interpretation of accumulation regularities for coal-enriched zones in Southwest China and structural settings for the deposit-formation of some metallic minerals by this viewpoint are summarized. Furthermore, three aspects of experience on the development of Chinese basic geological sciences and related applied sciences are expounded, and the direction and prospects for the "Chinese taphrogeny" research are forecasted.

油气藏地质及开发工程国家重点实验室资助

https://doi.org/10.11781/sysydz200102232