40Ar-39Ar and U-Pb ages of metadiorite from the East Kunlun Orogenic Belt: Evidence for Early-Paleozoic magmatic zone and excess argon in amphibole minerals-Reference-Cited by-同舟云学术

40Ar-39Ar and U-Pb ages of metadiorite from the East Kunlun Orogenic Belt: Evidence for Early-Paleozoic magmatic zone and excess argon in amphibole minerals

Published:2001-02 Issue:4 Volume:46 Page:330-333
ISSN:1001-6538
Container-title:Chinese Science Bulletin
language:en
Short-container-title:Chin.Sci.Bull.

Author:

Chen Nengsong,Sun Min,Zhang Kexin,Zhu Yunhai

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://link.springer.com/content/pdf/10.1007/BF03187197.pdf

Reference22 articles.

1. Lanphere, M. A., Dalrymple, G. B., Identification of excess40Ar by the40Ar-39Ar age spectrum technique, Earth and Planetary Science Letters, 1976, 32: 141.

2. Harrison, T. M., McDougall, I., Excess40Ar in metamorphic rocks from Broken Hill, New South Wales: Implications for40Ar-39Ar age spectra and the thermal history of the region, Earth and Planetary Science Letters, 1981, 55: 123.

3. Blanckenburg, F. V., Vilia, I. M., Argon retentivity and argon excess in amphiboles from the garbenschists of the Western Tauern Window, Eastern Alps, Contributions to Mineralogy and Petrology, 1988, 100: 1

4. Cliff, R. A., Rex, P. G., Guise, P. G., Geochronological studies of Proterozoic crustal evolution in the northern Outer Hebrides, Precambrian Research, 1998, 91: 401

5. Faure, G., Princeples of Isotope Geology, 2nd ed., New York: John Wiley & Sons, 1986.

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