How does the Chin state fit into the overall tectonic structure of Myanmar?
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The Chin state is part of the Indo-Myanmar Ranges (IMR) or the Indo-Burman Ranges (IBR), which extend from the East Himalayan Syntaxis (EHS) to the Andaman Sea. The IMR is located along the western margin of the Myanmar Microplate, between the Eurasian Plate and the Indian Plate. The tectonic structure of the Chin state is complex, as it lies in a zone of collision between the Indian and Asian plates and is north of the Sunda-Andaman subduction zone. The IMR in the Chin state is economically important, with occurrences of chromite and nickel deposits and submarine volcanic-hosted massive sulphide deposits. The tectonic history of the Chin state includes obduction of ophiolite nappe, subduction of the Indian Ocean, and extensional faulting.
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03 Nov 2021 1 Citations | The provided paper does not mention the Chin state or its tectonic structure in Myanmar. |
28 Mar 2022 | The provided paper does not mention the Chin state or its role in the overall tectonic structure of Myanmar. |
01 Jan 2022 1 Citations | The provided paper does not mention the Chin state or its tectonic structure in Myanmar. |
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