메뉴 건너뛰기




Volumn 319, Issue 5870, 2008, Pages 1654-1657

Sulfur and chlorine in late Cretaceous Deccan magmas and eruptive gas release

Author keywords

[No Author keywords available]

Indexed keywords

CHLORINE; SULFUR;

EID: 41149093602     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1152830     Document Type: Article
Times cited : (147)

References (29)
  • 5
    • 33750617042 scopus 로고    scopus 로고
    • 10.1029/2005JD006899
    • L. Oman et al., J. Geophys. Res. 111, D12209 10.1029/2005JD006899 (2006).
    • (2006) J. Geophys. Res , vol.111
    • Oman, L.1
  • 8
    • 0141522903 scopus 로고    scopus 로고
    • Th. Thordarson, S. Self, D. J. Miller, G. Larsen, E. G. Vilmundardottir, in Volcanic Degassing, C. Oppenheimer, D. M. Pyle, J. Barclay, Eds., 213 of Geological Society of London Special Publications (Geological Society of London, London, 2003), pp. 103-123.
    • Th. Thordarson, S. Self, D. J. Miller, G. Larsen, E. G. Vilmundardottir, in Volcanic Degassing, C. Oppenheimer, D. M. Pyle, J. Barclay, Eds., vol. 213 of Geological Society of London Special Publications (Geological Society of London, London, 2003), pp. 103-123.
  • 10
    • 41149168772 scopus 로고    scopus 로고
    • Materials and methods are available on Science Online.
    • Materials and methods are available on Science Online.
  • 12
    • 0035198679 scopus 로고    scopus 로고
    • T. Sano, T. Fujii, S. S. Deshmukh, T. Fukuoka, S. Aramaki, J. Petrol. 42, 2175 2001, These authors reported 0.6 wt, water in a glass inclusion, by FTIR. We have obtained an FTIR analysis of 0.5 wt, water in an olivine-hosted glass inclusion in sample MG4
    • T. Sano, T. Fujii, S. S. Deshmukh, T. Fukuoka, S. Aramaki, J. Petrol. 42, 2175 (2001). These authors reported 0.6 wt % water in a glass inclusion, by FTIR. We have obtained an FTIR analysis of 0.5 wt % water in an olivine-hosted glass inclusion in sample MG4.
  • 16
    • 41149096641 scopus 로고    scopus 로고
    • For a total mass of magma erupted, M, the mass of S released during degassing is MS,lost, M[(1, X chamber)Schamber, 1, X lava)Slava, 1) where Schamber and Slava are the S concentrations in the melt at depth, before any degassing as measured in the glass inclusions, and in the degassed matrix glass in the lava, respectively. X is the mass fraction of crystals present and is estimated by the amount of enrichment of an incompatible element with respect to the whole-rock concentration such that 1, Xchamber, Iwr/Iincl, where Iwr and Iincl are the concentrations of a highly incompatible element in the whole rock and in any nondegassed inclusion in which the sulfur value Schamber has been measured. Similarly, 1, Xlava
    • 2 contents are 1.55 wt % for MG4 and 1.29 wt % for MG5; see table S3.
  • 25
    • 11244266083 scopus 로고    scopus 로고
    • J. Grattan, Lithos 79, 343 (2005).
    • (2005) Lithos , vol.79 , pp. 343
    • Grattan, J.1
  • 29
    • 41149140465 scopus 로고    scopus 로고
    • We thank UK Natural Environment Research Council for funding this work grant NER/B/S/2003/00246, A. Jay for help with sample collection and geochemical analyses, and S. Sethna for general support of our fieldwork in India. We thank the four anonymous reviewers for their helpful comments
    • We thank UK Natural Environment Research Council for funding this work (grant NER/B/S/2003/00246), A. Jay for help with sample collection and geochemical analyses, and S. Sethna for general support of our fieldwork in India. We thank the four anonymous reviewers for their helpful comments.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.