A5018067713- Geological and Geochemical Analysis
- Hydrocarbon exploration and reservoir analysis
- Geochemistry and Geologic Mapping
- Geological and Geophysical Studies Worldwide
- earthquake and tectonic studies
- Geological and Tectonic Studies in Latin America
- Reservoir Engineering and Simulation Methods
- Geological and Geophysical Studies
- Geology and Paleoclimatology Research
- Paleontology and Stratigraphy of Fossils
- High-pressure geophysics and materials
- Groundwater and Isotope Geochemistry
- Geological formations and processes
- Archaeological and Historical Studies
- CO2 Sequestration and Geologic Interactions
- Archaeological and Geological Studies
- Mineral Processing and Grinding
- Heavy metals in environment
- Petroleum Processing and Analysis
- Coal and Its By-products
- Geochemistry and Elemental Analysis
- Enhanced Oil Recovery Techniques
- Clay minerals and soil interactions
- Astro and Planetary Science
- Urbanism, Landscape, and Tourism Studies
Repsol (Spain)
2010-2020
Technology Centre Prague
2019
Instituto de Geociencias
2006-2016
Universidad Nacional Autónoma de México
1999-2013
Autonomous University of Queretaro
2003-2013
Explora (Italy)
2010
Terra
2006
Nano Carbon (Poland)
2006
Mexican Geological Survey
2006
Universitat de Barcelona
1997-1998
Abstract Physical parameters of petroleum‐bearing fluid inclusions such as bulk density ( ρ ), molar volume V m vapour fraction ϕ vap ) and homogenization temperature T h are essential information to model petroleum composition x in reconstruct palaeotemperature palaeopressure trapping. For the main types contained a inclusion, we can follow how simultaneously influenced by change versus projection. We have correlated for different compositions large range values. However, postentrapment...
The Cierco Pb-Zn-Ag vein deposits, located in the central Pyrenees of Spain, crosscut Paleozoic metasedimentary rocks and are close proximity to Hercynian granodiorite dikes plutons. Galena sphalerite deposits have average delta 34 S values - 4.3 0.8 per mil (CDT), respectively. Coexisting mineral pairs give an isotopic equilibration temperature range 89 degrees 163 C which overlaps with 112 198 obtained from primary fluid inclusions. quartz has a 18 O value 19 + or 1 (VSMOW). deposited...
Abstract In the frontal part of south Pyrenean Eocene thrust-fault system, syn-kinematic fluid flow during early compressional deformation foreland basin marls is evidenced macroscopically by abundance calcite shear veins within zones and folds. The geometry distribution are indicative mechanisms kinematics fluid-deformation relationships, give assessment migration paths. crack-seal mechanism formation attests to episodic nature fault-slip associated in fractures. suggests that main source...
El carbón de Sonora, se localiza aproximadamente a 90 km al sur Hermosillo.La unidad portadora, tanto los mantos como del grafito, es la Formación Barranca Triásico, constituida por conglomerados, areniscas y limolitas rojas con intercalaciones lutitas grafito
La Perla is an Oligocene deposit of apatite iron ore located in northern Mexico. The main types are massive ore, breccia and powdery ore. latter special genetic interest because it contains well-preserved palynomorphs; fossil pollen representing several plant families growing the region investigation during late Paleogene-Neogene; assemblages include angiosperm gymnosperm grains, also fungal spores from two genera, Frasnacritetrus Dyctiosporites, indicative Eocene to Miocene age. beds...
Summary Brazilian Atlantic Passive Margins Basins have registered several volcanic events, which are very well documented in the most prolific offshore basins of Santos and Campos. Although, rocks usually not treated as potentials reservoir Brazil, they become important to Pre-Salt exploration, since been found Pre-salt exploration appraisal wells. These act only barriers for carbonate sedimentary successions but also potential reservoirs. Several wells drilled with properties significant...
The Taoudeni Basin (Mauritania / Mali, West Africa) was formed as a result of pre‐ Pan‐African subsidence associated with rifting at the margins African craton. Hydrocarbons in are derived from source rocks Meso‐Neoproterozoic Atar Group, which is composed facies varying stromatolite‐dominated carbonates to organic‐rich basinal shales. stromatolitic dolomitized and contain solid hydrocarbons (pyrobitumen). pyrobitumen response Mesozoic hydrothermal event, peak temperatures locally reaching...