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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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 |
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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 |
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© 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 |
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2019 |
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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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