Metamorphic garnet pyroxenite from the 540–600 m main borehole of the Chinese Continental Scientific Drilling (CCSD) project

作者: Lingsen Zeng , Fenghua Liang , Zhenyu Chen , Fulai Liu , Zhiqin Xu

DOI: 10.1016/J.TECTO.2009.02.043

关键词: Section (archaeology)EclogiteScientific drillingBoreholeGeochemistryGeologyUltramafic rockMaficOutcropMetamorphic rockEarth-Surface ProcessesGeophysics

摘要: Abstract Compared to other mafic and ultramafic rocks from the CCSD main borehole as well outcrops, 540–600 m section is extraordinary in terms of its geophysical geochemical properties. It consists > 70% hematite–ilmenite garnet pyroxenite (HI-GPX)

参考文章(63)
Bradley R. Hacker, J.G. Liou, William C. McClelland, Ultrahigh-pressure Metamorphism: Deep Continental Subduction ,(2006)
Ralph Kretz, Symbols for rock-forming minerals American Mineralogist. ,vol. 68, pp. 277- 279 ,(1983)
Alexander R. McBirney, Differentiation of the Skaergaard Intrusion Nature. ,vol. 253, pp. 691- 694 ,(1975) , 10.1038/253691A0
J.L Bodinier, M Guiraud, J Fabriés, J Dostal, C Dupuy, Petrogenesis of layered pyroxenites from the Lherz, Freychinéde and Prades ultramafic bodies (Ariége, French Pyrénées) Geochimica et Cosmochimica Acta. ,vol. 51, pp. 279- 290 ,(1987) , 10.1016/0016-7037(87)90240-7
Matthias G. Barth, William F. McDonough, Roberta L. Rudnick, Tracking the budget of Nb and Ta in the continental crust Chemical Geology. ,vol. 165, pp. 197- 213 ,(2000) , 10.1016/S0009-2541(99)00173-4
Florie A. Caporuscio, Joseph R. Smyth, Trace element crystal chemistry of mantle eclogites Contributions to Mineralogy and Petrology. ,vol. 105, pp. 550- 561 ,(1990) , 10.1007/BF00302494