Interpretation of the origin of massive replacive dolomite within atolls and submerged carbonate platforms: Strontium isotopic signature ODP Hole 866A, Resolution Guyot, Mid-Pacific Mountains

Sedimentary Geology

Volumn 101, Issue 1-2, 1996, Pages 9-13

  Flood, P G ^a   Fagerstrom, J A ^b   Rougerie, F ^c  

^a UNIVERSITY OF NEW ENGLAND   (Australia)

^b UNIVERSITY OF COLORADO   (United States)

^c Institut de Recherche pour le Developpement Papeete   (French Polynesia)

Author keywords

[No Author keywords available]

Indexed keywords

ATOLL; ATOLLS; CARBONATE PLATFORM; CARBONATE PLATFORMS; DIAGENESIS; DOLOMITIZATION; ENDO UPWELLING; ENDO-UPWELLING; HYDROTHERMAL FLOW; ISOTOPIC COMPOSITION; SR ISOTOPIC SIGNATURE; STRONTIUM; UPWELLING;

PACIFIC, MID-PACIFIC MOUNTAINS, RESOLUTION GUYOT; PACIFIC, RESOLUTION GUYOT, ODP HOLE 866A;

EID: 0029772606     PISSN: 00370738     EISSN: None     Source Type: Journal    
DOI: 10.1016/0037-0738(95)00098-4     Document Type: Article

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