0000000000890997

AUTHOR

Laurent Lambert

showing 2 related works from this author

Morphometry of micrite particles in cretaceous microporous limestones of the Middle East: influence on reservoir properties.

2011

24 pages; International audience; Microporosity may account for a significant part of the total porosity of Cretaceous limestone reservoirs of the Middle East. In these microporous facies porosity is moderate to excellent (up to 35%) while permeability is poor to moderate (up to 190 mD). Micritic limestones also may form dense layers with very low porosity and permeability values. Micritic samples were collected from three fields of the Habshan and Mishrif Formations, to examine the spatial relationship with their porosity, permeability and pore throat radius distributions. Two key parameters of the micritic particles are studied using scanning electron microscopy: their morphology (shape a…

Micrite010504 meteorology & atmospheric sciencesMicriteScanning electron microscopeStratigraphy[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/PetrographyCarbonatesMineralogy010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousPermeabilityMiddle EastMicroporosityPorosity0105 earth and related environmental sciences[ SDU.STU.PE ] Sciences of the Universe [physics]/Earth Sciences/PetrographyPetrophysicsGeologyMicroporous materialCretaceousPermeability (earth sciences)Geophysics[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesEconomic GeologyGeology
researchProduct

Burial dissolution of micrite in Middle East carbonate reservoirs (Jurassic–Cretaceous): keys for recognition and timing.

2006

14 pages; International audience; This paper discusses burial diagenesis and especially a burial dissolution phase and its effects on micrite microtexture in reservoirs in the Middle East. Three microporous reservoirs were selected: the Cenomanian Mishrif Formation in Iraq; the Kimmeridgian–Tithonian Arab D and the Barremian Kharaib Formations, both in Abu Dhabi. Staining, cathodoluminescence and scanning electron microscopy were used for petrographic observations. In the selected reservoirs, three typical micrite microtextures are distinguished: micro-rhombic, compact anhedral, and rounded. The chronology of diagenesis, based on petrographic observations, shows that mineralogical stabilisa…

CalciteCarbonate reservoirMicriteMicriteStratigraphyMineralogyGeologyOceanographyCementation (geology)[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryDiagenesisDiagenesisPetrographychemistry.chemical_compoundMiddle East[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicschemistryCarbonate rockCarbonateEconomic GeologySedimentary rockGeology[ SDU.STU.PE ] Sciences of the Universe [physics]/Earth Sciences/Petrography
researchProduct