Comment on: Discovery of the fossiliferous Cu Brei Formation (Lower Devonian) in the Kon Tum Block (South Viet Nam): Tong-Dzuy Thanh, Than Duc Duyen, Nguyen Huu Hung, Bui Phu My

Henri Maluski

doi:10.1016/j.jseaes.2007.09.002

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Comment on: Discovery of the fossiliferous Cu Brei Formation (Lower Devonian) in the Kon Tum Block (South Viet Nam): Tong-Dzuy Thanh, Than Duc Duyen, Nguyen Huu Hung, Bui Phu My

Journal article

Peer reviewed

Comment on: Discovery of the fossiliferous Cu Brei Formation (Lower Devonian) in the Kon Tum Block (South Viet Nam): Tong-Dzuy Thanh, Than Duc Duyen, Nguyen Huu Hung, Bui Phu My

Henri Maluski

Journal of Southeast Asian earth sciences, Vol.31(4-6), pp.562-563

2008

DOI: https://doi.org/10.1016/j.jseaes.2007.09.002

Abstract

metamorphism

Kon Tum massif

Truong son belt

massif

ages

The publication of Tong-Dzuy Thanh et al. calls for two remarks: The metamorphism in the "Kon Turn block" cannot be younger than Permian because the outcrop they describe is not metamorphic. Their very interesting discovery is a new piece of evidence for the exotic origin of the Dien Binh Series. (c) 2007 Elsevier Ltd. All rights reserved.

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Title: Comment on: Discovery of the fossiliferous Cu Brei Formation (Lower Devonian) in the Kon Tum Block (South Viet Nam): Tong-Dzuy Thanh, Than Duc Duyen, Nguyen Huu Hung, Bui Phu My
Creators - without role: Henri Maluski - Université de Montpellier, Géosciences Montpellier - GM
Publication Details: Journal of Southeast Asian earth sciences, Vol.31(4-6), pp.562-563
Identifiers: 9944913909311
Academic Unit: Géosciences Montpellier - GM
Language: English
Resource Type: Journal article
Local Fields: hal-00411445