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Volumn 30, Issue 6, 2002, Pages 499-502

Slab-derived fluids and quartz-vein formation in an accretionary prism, Otago Schist, New Zealand

Author keywords

Accretionary prism; Au W mineralization; Fluid flow; New Zealand; Otago Schist; Quartz veins

Indexed keywords

FLUIDS; METAMORPHIC ROCKS; QUARTZ; SEDIMENTS; SILICA;

EID: 84874994934     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(2002)030<0499:SDFAQV>2.0.CO;2     Document Type: Article
Times cited : (108)

References (23)
  • 2
    • 3843092185 scopus 로고
    • Mass transfer during Barrovian metamorphism of pelites, south-central Connecticut: II. Channelized fluid flow and the growth of staurolite and kyanite
    • (1994) American Journal of Science , vol.294 , pp. 1061-1134
    • Ague, J.J.1
  • 5
    • 0030391537 scopus 로고    scopus 로고
    • Assessing metasomatic mass and volume changes using the bootstrap, with application to deep crustal hydrothermal alteration of marble
    • (1996) Economic Geology , vol.91 , pp. 1169-1182
    • Ague, J.J.1    van Haren, J.L.M.2


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.