Lower crustal assimilation revealed by sulfur isotope systematics of the Bear Valley Intrusive Suite, southern Sierra Nevada Batholith, California, USA
Author:
Funder
Swiss National Foundation Postdoc Mobility Grant
National Science Foundation
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00410-024-02123-2.pdf
Reference121 articles.
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2. Ague JJ, Brimhall GH (1988) Magmatic arc asymmetry and distribution of anomalous plutonic belts in the batholiths of California: effects of assimilation, crustal thickness, and depth of crystallization. Bull Geol Soc Am 100:912–927. https://doi.org/10.1130/0016-7606(1988)100<0912:MAAADO>2.3.CO;2
3. Alt JC, Shanks WC, Jackson MC (1993) Cycling of sulfur in subduction zones: the geochemistry of sulfur in the Mariana Island Arc and back-arc trough. Earth Planet Sci Lett 119:477–494. https://doi.org/10.1016/0012-821X(93)90057-G
4. Annen C, Blundy JD, Sparks RSJ, Gene DE (2006) The Genesis of Intermediate and Silicic Magmas in Deep Crustal Hot zones. J Petrol 47:505–539. https://doi.org/10.1093/petrology/egi084
5. Aster EM, Wallace PJ, Moore LR, Watkins J, Gazel E, Bodnar RJ (2016) Reconstructing CO2 concentrations in basaltic melt inclusions using Raman analysis of vapor bubbles. J Volcanol Geotherm Res 323:148–162. https://doi.org/10.1016/j.jvolgeores.2016.04.028
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