The role of strike-slip faulting in the history of the Hukawng Block and the Jade Mines Uplift, Myanmar

© 2019 The Geologists' Association The Hukawng Basin is bounded on its east by splays of the still-active Sagaing Fault. Palinspastically restoring Myanmar's blocks to their positions before the widely-accepted c.400 km dextral strike-slip fault displacement, places the Hukawng Block along...

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Main Authors: Michael F. Ridd, Michael J. Crow, Christopher K. Morley
Format: Journal
Published: 2019
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http://cmuir.cmu.ac.th/jspui/handle/6653943832/63637
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Institution: Chiang Mai University
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spelling th-cmuir.6653943832-636372019-03-18T02:22:27Z The role of strike-slip faulting in the history of the Hukawng Block and the Jade Mines Uplift, Myanmar Michael F. Ridd Michael J. Crow Christopher K. Morley Earth and Planetary Sciences © 2019 The Geologists' Association The Hukawng Basin is bounded on its east by splays of the still-active Sagaing Fault. Palinspastically restoring Myanmar's blocks to their positions before the widely-accepted c.400 km dextral strike-slip fault displacement, places the Hukawng Block alongside the Tengchong Block, suggesting they were formerly connected. Additionally the Cretaceous–Paleogene Medial-Myanmar Shear Zone then aligns with the NW-SE Jade Mines Belt. Jadeitite formed there under HP/LT conditions in a Mesozoic subduction zone. It was exhumed at the intersection of the dextral Medial-Myanmar Shear Zone with the subduction-zone at the continental margin of Sundaland. The later Sagaing Fault played no part in that exhumation. 2019-03-18T02:22:27Z 2019-03-18T02:22:27Z 2019-01-01 Journal 00167878 2-s2.0-85061567418 10.1016/j.pgeola.2019.01.002 https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85061567418&origin=inward http://cmuir.cmu.ac.th/jspui/handle/6653943832/63637
institution Chiang Mai University
building Chiang Mai University Library
country Thailand
collection CMU Intellectual Repository
topic Earth and Planetary Sciences
spellingShingle Earth and Planetary Sciences
Michael F. Ridd
Michael J. Crow
Christopher K. Morley
The role of strike-slip faulting in the history of the Hukawng Block and the Jade Mines Uplift, Myanmar
description © 2019 The Geologists' Association The Hukawng Basin is bounded on its east by splays of the still-active Sagaing Fault. Palinspastically restoring Myanmar's blocks to their positions before the widely-accepted c.400 km dextral strike-slip fault displacement, places the Hukawng Block alongside the Tengchong Block, suggesting they were formerly connected. Additionally the Cretaceous–Paleogene Medial-Myanmar Shear Zone then aligns with the NW-SE Jade Mines Belt. Jadeitite formed there under HP/LT conditions in a Mesozoic subduction zone. It was exhumed at the intersection of the dextral Medial-Myanmar Shear Zone with the subduction-zone at the continental margin of Sundaland. The later Sagaing Fault played no part in that exhumation.
format Journal
author Michael F. Ridd
Michael J. Crow
Christopher K. Morley
author_facet Michael F. Ridd
Michael J. Crow
Christopher K. Morley
author_sort Michael F. Ridd
title The role of strike-slip faulting in the history of the Hukawng Block and the Jade Mines Uplift, Myanmar
title_short The role of strike-slip faulting in the history of the Hukawng Block and the Jade Mines Uplift, Myanmar
title_full The role of strike-slip faulting in the history of the Hukawng Block and the Jade Mines Uplift, Myanmar
title_fullStr The role of strike-slip faulting in the history of the Hukawng Block and the Jade Mines Uplift, Myanmar
title_full_unstemmed The role of strike-slip faulting in the history of the Hukawng Block and the Jade Mines Uplift, Myanmar
title_sort role of strike-slip faulting in the history of the hukawng block and the jade mines uplift, myanmar
publishDate 2019
url https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85061567418&origin=inward
http://cmuir.cmu.ac.th/jspui/handle/6653943832/63637
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