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

Liu Chenming; Yang Demin

doi:doi:10.11648/j.earth.20180702.13

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

Liu Chenming, Yang Demin

Published in Earth Sciences (Volume 7, Issue 2)

Received: 21 January 2018 Accepted: 3 February 2018 Published: 5 March 2018

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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.

Published in	Earth Sciences (Volume 7, Issue 2)
DOI	10.11648/j.earth.20180702.13
Page(s)	58-63
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2018. Published by Science Publishing Group

Keywords

ELIP, LIPs, Meteorite Impact, Basalt, Paleogeography, Collisions Aggregation Effect, Basalts

References

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Liu Chenming, Yang Demin. (2018). Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”. Earth Sciences, 7(2), 58-63. https://doi.org/10.11648/j.earth.20180702.13

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Liu Chenming; Yang Demin. Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”. Earth Sci. 2018, 7(2), 58-63. doi: 10.11648/j.earth.20180702.13

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AMA Style

Liu Chenming, Yang Demin. Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”. Earth Sci. 2018;7(2):58-63. doi: 10.11648/j.earth.20180702.13

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@article{10.11648/j.earth.20180702.13,
  author = {Liu Chenming and Yang Demin},
  title = {Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”},
  journal = {Earth Sciences},
  volume = {7},
  number = {2},
  pages = {58-63},
  doi = {10.11648/j.earth.20180702.13},
  url = {https://doi.org/10.11648/j.earth.20180702.13},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20180702.13},
  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.},
 year = {2018}
}

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TY  - JOUR
T1  - Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”
AU  - Liu Chenming
AU  - Yang Demin
Y1  - 2018/03/05
PY  - 2018
N1  - https://doi.org/10.11648/j.earth.20180702.13
DO  - 10.11648/j.earth.20180702.13
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 58
EP  - 63
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20180702.13
AB  - 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.
VL  - 7
IS  - 2
ER  -

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Author Information

Liu Chenming

Resource Exploration Institute, Yunnan Land and Resources Vocational College, Kunming, China
Yang Demin

Resource Exploration Institute, Yunnan Land and Resources Vocational College, Kunming, China

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Liu Chenming, Yang Demin. (2018). Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”. Earth Sciences, 7(2), 58-63. https://doi.org/10.11648/j.earth.20180702.13

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ACS Style

Liu Chenming; Yang Demin. Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”. Earth Sci. 2018, 7(2), 58-63. doi: 10.11648/j.earth.20180702.13

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AMA Style

Liu Chenming, Yang Demin. Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”. Earth Sci. 2018;7(2):58-63. doi: 10.11648/j.earth.20180702.13

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@article{10.11648/j.earth.20180702.13,
  author = {Liu Chenming and Yang Demin},
  title = {Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”},
  journal = {Earth Sciences},
  volume = {7},
  number = {2},
  pages = {58-63},
  doi = {10.11648/j.earth.20180702.13},
  url = {https://doi.org/10.11648/j.earth.20180702.13},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20180702.13},
  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.},
 year = {2018}
}

Copy | Download

TY  - JOUR
T1  - Research on Paleogeography Recovery of "Impact Point" Based on “Collisions Aggregation Effect”
AU  - Liu Chenming
AU  - Yang Demin
Y1  - 2018/03/05
PY  - 2018
N1  - https://doi.org/10.11648/j.earth.20180702.13
DO  - 10.11648/j.earth.20180702.13
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 58
EP  - 63
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20180702.13
AB  - 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.
VL  - 7
IS  - 2
ER  -

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