M. Reyes

ORCID: 0000-0003-1306-7389
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About
Contact & Profiles
Research Areas
  • Geological and Tectonic Studies in Latin America
  • Ionosphere and magnetosphere dynamics
  • Geophysics and Gravity Measurements
  • Geomagnetism and Paleomagnetism Studies
  • Earthquake Detection and Analysis
  • earthquake and tectonic studies
  • Cancer Treatment and Pharmacology
  • GNSS positioning and interference
  • Advanced Research in Science and Engineering
  • Magnetic Field Sensors Techniques
  • Geochemistry and Geologic Mapping
  • Geological Modeling and Analysis
  • Botany and Geology in Latin America and Caribbean
  • Astro and Planetary Science
  • Space Satellite Systems and Control
  • Statistical and numerical algorithms
  • Seismic Imaging and Inversion Techniques
  • Seismology and Earthquake Studies

University of Göttingen
2021-2024

Universidad Autónoma de Bucaramanga
2022

Ecopetrol (Colombia)
2016

Instituto Colombiano del Petróleo y Energías de la Transición - Icpet
2016

Acute Coronary Syndrome (ACS) remains a significant global burden, necessitating ongoing innovation in therapeutic strategies. Over the past three decades, landmark clinical trials such as PRISM, PRISM-PLUS, PARAGON A, B, PURSUIT, and GUSTO IV-ACS have shaped our understanding management of ACS. These studies provided pivotal data on role antithrombotic agents, glycoprotein IIb/IIIa inhibitors, tailored approaches high-risk populations. This review explores design, outcomes, impact these...

10.47191/ijmscrs/v5-i03-05 article EN cc-by International Journal of Medical Science and Clinical Research Studies 2025-03-10

Abstract Before the rise of Northern Andes in Cenozoic time, Triassic to Jurassic extensional basins northwestern South America accommodated predominantly continental strata partly intercalated with volcanic rocks. Coeval plutonism is attributed a magmatic arc related subduction Farallon plate beneath America. The later became involved Andean orogeny and are now partially exposed Eastern Cordillera Middle Magdalena Valley Colombia. We have employed (U/Pb) geochronology on zircons from...

10.1007/s00531-024-02441-7 article EN cc-by International Journal of Earth Sciences 2024-07-06

We have developed a new method to assess the movement of particles in different steps well-calibrated sequential kinematic restoration. Calibration included correct assessment amounts overburden, sedimentation, erosion, and thermal behavior through time. Our allowed better understanding mechanisms deformation uplift geologic provinces. In our pilot case study Colombian Eastern Cordillera, we used vectors balanced cross sections document an initial phase dominant vertical final tangential...

10.1190/int-2015-0049.1 article EN Interpretation 2016-02-01

The present-day Magdalena Valley, Eastern Cordillera, and Llanos Basin were part of a regional multiphase basin that started as an extensional in the Jurassic. Then, it was transformed into retroarc foreland Late Cretaceous subsequently separated hinterland during late Eocene. We incorporated new data from Cordillera chronostratigraphically correlated with adjacent basins. Their correlation contributed to establishing stratigraphic boundaries formed first-order changes marked beginning end...

10.3389/feart.2022.876140 article EN cc-by Frontiers in Earth Science 2022-09-12

Along the Colombian Llanos Foothills, different rock formations lie affected by tectonic movements, expressing geomorphological changes at surface associated with subsurface geologic structures (anticlines and synclines). Some of them were created during most recent movements throughout last period geological time. This evidence is plotted in map area extended from Eastern Cordillera to Orientales basin (figure 1). There, folded faulted Quaternary deposits can be observed. case alluvial...

10.1071/aseg2016ab239 article EN ASEG Extended Abstracts 2016-12-01

Summary The Eastern Cordillera is bounded by the Middle Magdalena Valley basin in west and Llanos Foothills to east. It commonly interpreted have grown from a Mesozoic rift that became inverted during Cenozoic Andean orogeny both eastern western margins of were thrust over adjacent basins inversion, resulting complex combination thick-skinned thin-skinned structures. geological evolution study area key understanding structural configuration related such as Valley. influence on geometry syn...

10.3997/2214-4609.202012018 article EN 2021-01-01
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