María del Carmen Ayora Esteban

ORCID: 0000-0001-8467-7411
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About
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Research Areas
  • Spanish Linguistics and Language Studies
  • Geological and Geophysical Studies Worldwide
  • Geological and Geophysical Studies
  • Hydrocarbon exploration and reservoir analysis
  • Language, Linguistics, Cultural Analysis
  • Literacy and Educational Practices
  • Geological formations and processes
  • Linguistic and Sociocultural Studies
  • Linguistic Studies and Language Acquisition
  • Organ Transplantation Techniques and Outcomes
  • Renal Transplantation Outcomes and Treatments
  • Hydraulic Fracturing and Reservoir Analysis
  • Coral and Marine Ecosystems Studies
  • Reservoir Engineering and Simulation Methods
  • Paleontology and Stratigraphy of Fossils
  • Organ Donation and Transplantation
  • Geological and Tectonic Studies in Latin America
  • Gender and Feminist Studies
  • Karst Systems and Hydrogeology
  • Archaeological and Historical Studies
  • History of Education in Spain
  • Enhanced Oil Recovery Techniques
  • Geological Studies and Exploration
  • Immigration and Intercultural Education
  • African Studies and Geopolitics

Universidad de Granada
2002-2019

Complejo Hospitalario de Salamanca
2018

Instituto de Investigación Biomédica de Salamanca
2018

Universidad de Salamanca
2018

Repsol (Spain)
2010-2015

Hospital Universitario Virgen de las Nieves
2012

Abstract Major corrosion has been found at depth in carbonate hydrocarbon reservoirs from different geologic provinces. Fluid inclusion microthermometry and stable isotopic compositions of cements, predating major corrosion, constrain the interpretation evolution parental fluids during progressive burial prior to event. Post‐major mineral paragenesis includes pyrite (‐marcasite), anhydrite, kaolinite (dickite) fluorite. Although post‐corrosion represents minor volumes rock, it may provide...

10.1111/j.1468-8123.2006.00167.x article EN Geofluids 2007-02-16

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...

10.3997/2214-4609.201412890 article EN Proceedings 2015-05-26

This paper presents a geological map and cross-section of the Falcón Basin based both on published unpublished work new data collected in northern southern basin margins. The covers an area 4600 km2 at 1:100,000 scale. is oriented NNW-SSE, traversing perpendicular to main structures. In general, structure study results from inversion graben (Oligocene-early Miocene back-arc basin), that started middle due convergence between Caribbean South American plates. map, observations made field have...

10.1080/17445647.2017.1333969 article EN cc-by Journal of Maps 2017-06-07

Summary Pre-salt carbonate reservoirs in the offshore Campos and Santos basins have played a crucial role over last years with giant discoveries being made every year. The overall pre-salt account for 28.8 BBls RR twelve fields currently producing 648,000 b/d from carbonates. present an heterogeneous variation that can range thick packages of microbial sections, interbedded sequences carbonates volcanics or complete absence reservoir facies. Moreover, diagenetic processes, such as...

10.3997/2214-4609.201412891 article EN Proceedings 2015-05-26

Rock properties of the Natih Formation in Field F were strongly modified as a result diagenesis. The paragenetic sequence is well defined, and typical for carbonate field from this geographic location time period. It exhibits an interplay between early diagenetic processes, faulting tectonically controlled circulation deep burial fluids. Conclusions are supported by detailed petrographic geochemical data including isotopes, fluid inclusions elemental compositions.

10.3997/2214-4609.20145357 article EN Proceedings 2010-01-24

10.1177/0218492311435922 article EN Asian Cardiovascular and Thoracic Annals 2012-10-01

It is commonly considered that reservoir properties of Peritethyan carbonates mostly originated<br>from intense dissolution (vugs, molds, enlarged fractures, caverns) in a variety meteoric<br>diagenetic environments. This took place prior to the burial by non-reservoir or seal<br>units, under unconformities different orders magnitude shallow, near-surface aquifers.<br>Primary depositional porosities are seen as extensively obliterated cementation and<br>compaction.

10.3997/2214-4609.201405769 article EN 2002-01-01

Summary Evaporite basins are commonly rimmed by a wide range of facies made complex depositional lithologies later affected various diagenetic processes along the basin margins in response to recurrent fluctuations relative sea level and associated water chemistry. The example Messinian SE Spain is presented as potential reference model for other salt basins.

10.3997/2214-4609.201413562 article EN Proceedings 2015-05-26
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