Permian-Triassic Magmatism in the Qin-Fang Tectonic Belt, SW China: New Insights into Tectonic Evolution of the Eastern Paleo-Tethys
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12583-020-1111-6.pdf
Reference63 articles.
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2. Cai, Y. F., Liu, H. C., Feng, Z. H., et al., 2020. Neoproterozoic Active Margin of the SW South China Block: Constraints from U-Pb Ages, Sr-Nd Isotopes and Geochemical Data for the Gabbro and Granodiorite along the Ailaoshan Tectonic Belt. Lithos, 358/359: 105387. https://doi.org/10.1016/j.lithos.2020.105387
3. Cai, Y. F., Wang, Y. J., Cawood, P. A., et al., 2014. Neoproterozoic Subduction along the Ailaoshan Zone, South China: Geochronological and Geochemical Evidence from Amphibolite. Precambrian Research, 245: 13–28. https://doi.org/10.1016/j.precamres.2014.01.009
4. Champion, D. C., Bultitude, R. J., 2013. The Geochemical and Sr-Nd Isotopic Characteristics of Paleozoic Fractionated S-Types Granites of North Queensland: Implications for S-Type Granite Petrogenesis. Lithos, 162/163: 37–56. https://doi.org/10.1016/j.lithos.2012.11.022
5. Chappell, B. W., White, A. J. R., 1974. Two Contrasting Granite Types. Pacific Geology, 8: 173–174
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