Reconstruction of the fluid flow history during Laramide foreland fold and thrust belt development in eastern Mexico: Cathodoluminescence and δ18O-δ13C isotope trends of calcite-cemented fractures

Journal of Geochemical Exploration

Volumn 78-79, Issue , 2003, Pages 163-167

  Ferket, H ^a   Swennen, R ^a   Ortuno S ^b   Roure, F ^c  

^a UNIVERSITY OF LEUVEN   (Belgium)

^b INSTITUTO MEXICANO DEL PETRÓLEO   (Mexico)

^c IFP ENERGIES NOUVELLES   (France)

Author keywords

Diagenesis; Fluid flow; Foreland fold and thrust belt; Reservoir

Indexed keywords

CATHODOLUMINESCENCE; HYDRAULIC FRACTURING; ISOTOPES; PETROLEUM RESERVOIRS; ROCKS;

DIAGENESIS; FORELAND FOLDS; HYDROCARBON RESERVOIRS; THRUST BELTS;

FLOW OF FLUIDS;

CALCITE; CATHODOLUMINESCENCE; DIAGENESIS; FLUID FLOW; FOLD AND THRUST BELT; FORELAND BASIN; FRACTURE; HOST ROCK; HYDRAULIC FRACTURE; HYDROCARBON MIGRATION; HYDROCARBON RESERVOIR; ISOTOPIC ANALYSIS; KARST; RECOGNITION; RESERVOIR ROCK; STABLE ISOTOPE;

CORDOBA PLATFORM; MEXICO [NORTH AMERICA]; NORTH AMERICA; VERACRUZ;

EID: 20744438198     PISSN: 03756742     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0375-6742(03)00119-5     Document Type: Conference Paper

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