Dating thin zircon rims by NanoSIMS: The Fengtien nephrite (Taiwan) is the youngest jade on Earth

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Title:	Dating thin zircon rims by NanoSIMS: The Fengtien nephrite (Taiwan) is the youngest jade on Earth
Authors:	陳致同;Yui, Tzen-Fu;Usuki, Tadashi;Chen, Chun-Yen;Ishida, Akizumi;Sano, Yuji;Suga, Kenshi;Iizuka, Yoshiyuki;Chen, Chih-Tung
Contributors:	地球科學學院地球科學學系
Keywords:	Earth;Geological time;Isotopes;NanoSIMS;nephrite;Taiwan;U-Pb dating;zircon
Date:	2014-01-01
Issue Date:	2026-04-23 11:31:42 (UTC+8)
Publisher:	Taylor and Francis Ltd.;Philadelphia: Taylor & Francis
Abstract:	摘要： Nephrite in the Fengtien area of the eastern part of the Central Mountain Range, Taiwan, is associated with antigorite-serpentinite within the Yuli belt, a late Cenozoic subduction-accretionary complex related to the eastward subduction of the South China Sea plate forming the Luzon arc. Diopsidite and clinozoisite rock are two other metasomatic components accompanying nephrite between serpentinites and the greenschist-facies country rock (carbonaceous material-)quartz-mica schist. Detrital zircons were separated from one clinozoisite rock sample, formed through metasomatic replacement after mica-quartz schist at temperatures of 320-420°C or slightly lower, which is lower than the metamorphic temperature conditions of the Yuli belt. Most of the detrital zircons have thin zircon rims less than 15-20 μm wide. These zircon rims, considered as newly formed during metasomatism leading to nephrite/diopsidite/clinozoisite rock formation, were dated by a high lateral resolution secondary ion mass spectrometer (CAMECA NanoSIMS NS50). The resulting 238 U/ 206 Pb- 204 Pb/ 206 Pb inverse isochron gave an age of 3.3 ± 1.7 Ma. The collision of the Eurasian continental margin with the Luzon arc has been suggested to have begun at ca. 6.5 Ma in the Taiwan area. The nephrite formation processes therefore clearly post-dated South China Sea plate subduction. The present date, substantiated by the metamorphic and metasomatic temperature information, demonstrates that the fluid-rock interaction forming Fengtien nephrite would have taken place during a Barrovian-type metamorphic overprint resulting from arc-continent collision, leading to the exhumation of the Yuli belt. This conclusion on nephrite formation with regard to regional tectonics can serve as a working model for future studies on other nephrite deposits with similar occurrences, mostly embedded within Mesozoic or older subduction-accretionary complexes. The Fengtien nephrite deposit is therefore the youngest one of its kind exposed on Earth's surface. 出版者： Philadelphia: Taylor & Francis 出版日期： 2014-12-10 出處： International Geology Review, 2014-12, Vol.56 (16), p.1932-1944 版權： 2014 Taylor & Francis 2014 版權： 2014 Taylor & Francis 識別號： ISSN: 0020-6814 識別號： EISSN: 1938-2839 識別號： DOI: 10.1080/00206814.2014.972994
Appears in Collections:	[Department of Earth Sciences ] journal & Dissertation

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