[Comment] New zircon radiometric U-Pb ages and Lu-Hf isotopic data from the ultramafic-mafic sequences of Ranau and Telupid (Sabah, eastern Malaysia): Time to reconsider the geological evolution of Southeast Asia?

Cullen, A.; Burton-Johnson, A. ORCID: https://orcid.org/0000-0003-2208-0075. 2021 [Comment] New zircon radiometric U-Pb ages and Lu-Hf isotopic data from the ultramafic-mafic sequences of Ranau and Telupid (Sabah, eastern Malaysia): Time to reconsider the geological evolution of Southeast Asia? Geology, 49 (11), e541. 541. 10.1130/G49414C.1

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Abstract/Summary

Tsikouras et al. (2021) interpret Miocene zircon U-Pb ages from ophiolitic rocks in Sabah, Malaysia, as magmatic ages related to southwest propagation of Sulu Sea spreading into onshore Borneo, even though the ophiolites and associated intrusions east of Telupid yield Mesozoic ages (Graves et al., 2000; Burton-Johnson et al., 2020). For the following five reasons, we believe these new zircon ages have been misrepresented to fit a tectonic model:

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1130/G49414C.1
ISSN:	00917613
Date made live:	15 Nov 2021 12:23 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/531384

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1130/G49414C.1

ISSN:

00917613

Date made live:

15 Nov 2021 12:23 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/531384