Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”

Li Chenming, Yang Demin
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引用次数: 2

Abstract

In 2015 and 2018, the author put forward the new hypothesis of the origin to the Emeishan LIP based on the “Collisions Aggregation Effect” of a Meteorite Impact. Under the guidance of this hypothesis, the author and his team collected a large number of domestic and international researches on Emeishan LIP and paleogeography, it is concluded that: 1. The main eruptive period of ELIP is at the P/Tr boundary period, about 257Ma. Its main distribution is located at 4°S, 152°E or 4°S, 110°E, located in YZ Block of the Southwest China, and is the marine facies eruption. 2. Based on the “Collisions Aggregation Effect”, the author proposed that the "impact point" is located in the 4°N, 28°W or 4°N, 70°W at the P/Tr boundary period, and is the marine sedimentary environment; 3. Combined with the "impact point" paleogeographic location, put forward located in the Atlantic Ocean of the northeastern Brazil or Colombia now; 4. The author believes that the"impact point" just in the oceans at the P/Tr boundary period, It is possible that the "impact point" of a meteorite is located exactly in the Panthalassic Ocean, resulting in an extensive regression, significant sea level declines, over 90% of marine life, and nearly 70% of the land extinction? 5. The authors will further study and analyze the evolution of the Panthalassic Ocean in the hope of gaining some ground from it, hoping to find evidence to verify the "impact point" and hope that interested researchers can join in to participate in the work.
基于“碰撞聚集效应”的“撞击点”古地理恢复研究
2015年和2018年,作者基于一次陨石撞击的“碰撞聚集效应”,提出了峨眉山LIP起源的新假说。在这一假设的指导下,作者及其团队收集了大量国内外关于峨眉山LIP和古地理的研究成果,得出以下结论:ELIP的主要喷发期在P/Tr边界期,约为257Ma。其主要分布于东经4°S 152°或东经4°S 110°,位于西南YZ地块,为海相喷发。2. 基于“碰撞聚集效应”,作者提出“撞击点”位于P/Tr边界期4°N、28°W或4°N、70°W,为海相沉积环境;3.结合“撞击点”的古地理位置,提出现在位于巴西或哥伦比亚的大西洋东北部;4. 笔者认为,陨石的“撞击点”恰好在P/Tr边界期的海洋中,有可能陨石的“撞击点”恰好位于泛海相洋,造成大面积回归,海平面明显下降,90%以上的海洋生物,近70%的陆地生物灭绝。5. 作者将进一步研究和分析泛海的演化,希望能从中有所收获,希望能找到证据来验证“冲击点”,希望有兴趣的研究者能加入进来参与工作。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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