GOLFO DE MÉXICO
Marisol Mirari Atela Castillo
Created on November 13, 2023
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Transcript
Presenta: Usama Ismael Yarbuh Lugo
UNIVERSIDAD Autónoma de Baja California FACUltad de Ciencias Marinas OCEANOGRAFÍA DE MARES DE MÉXICO
Fold development and Syn-tectonic sedimentation Patterns in the Gulf of Mexico
Deep-water passive margin foldbelts around the world
Location of deep-water passive margin foldbelts around the world. From Morley (2011).
DEEP-WATER FOLDING
Salt tectonics. From Fossen (2010)
Detachment folding. From Fossen (2010)
Detachment folds vs salt tectonic folds
DEEP-WATER FOLDING
Fault-propagation fold
Detachment fold
Fault-bend fold
Other types of folds
DEEP-WATER FOLDING
Hydrocarbon generation window. From https://infolupki.pgi.gov.pl/en/gas/thermal-maturity-organic-matter-and-gas-exploration)
Folds in the oil industry
DEEP-WATER Oil exploration
Cartoon showing a petroleum system. From Kundu (2023)
From Valls (2015)
Is a back-arc basin
THE GULF OF MEXICO
Abyssal plain
Veracruz shelf
Campeche scarpment
Sigsbee scarpment
Yucatan shelf
Florida shelf
Mississippi shelf
Fromhttps://atlascigom.cicese.mx/map_data/T000/ATLAS-TOMO-0.pdf
Bathymetry
General setting of the Gulf of Mexico
Fromhttps://atlascigom.cicese.mx/map_data/T000/ATLAS-TOMO-0.pdf
Physiographic provinces
General setting of the Gulf of Mexico
Gondwana
Laurasia
- Pangea fragmentation (Upper Paleozoic-Lower Mesozoic).
- Continental shale deposits during the Mesozoic.
- Marine water invasion.
- High evaporation.
- High volumes of salt deposits during the Jurassic forming evaporites.
- Carbonate sedimentation during from Late Jurassic to Late Cretaceous.
From Naugen and Mann (2015).
Of the Golf of Mexico
TECTONIC EVOLUTION
- Thermal subsidence during the Cretaceous.
- Uplift of the Sierra Madre Oriental (Laramide Orogeny).
- Clastic sedimentation from Paleogene filling the basin (hemipelagic and turbiditie systems).
- Tectonic inversion
- Foldbelt devolpment.
From Trudgill et al. (1999).
TECTONIC EVOLUTION
Foldbelt distribution in the Golf of Mexico
Kenning and Manning (2020).
TECTONIC EVOLUTION
Regional map showing the main structural features of the southwestern Gulf of Mexico basin. From Yarbuh et al. (2018) .
The Mexican Ridges foldbelt
Case study
The Mexican Ridges foldbelt
Case study
From Yarbuh and Contreras (2015)
Case study
From Yarbuh et al. (2018)
Case study
Structural parameters of a detachment fold. From Yarbuh and Contreras (2015).
Geometry of folds
Case study
Example for fold No. 7 of the MRFB. From Yarbuh and Contreras (2015).
The Area-Depth-Strain Analysis
Case study
Examples for folds No. 1 and 6. From Yarbuh and Contreras (2015).
The Area-Depth-Strain Analysis
Case study
From Yarbuh and Contreras (2015).
Deformation started synchronously during the Late Miocene throughout the MRFB
Results. The onset of deformation in the MRFB
Case study
From Yarbuh and Contreras (2015).
Total shortening of 11.8 km
Results. Shortening
Case study
From Yarbuh and Contreras (2015).
Tectonic uplif decreases with distance
Results. Tectonic uplift
Case study
Sedimentation rate decreases with distance
From Yarbuh and Contreras (2015).
Results. Sedimentation rate
Case study
Mass movement towards the fold crest. From Lotero-Velez et al. (2019)
From Yarbuh and Contreras (2015).
Results. Mass diffusion coefficient
Case study
Dr. Ismael Yarbuh Profesor ordinario de carrera titular nivel “B” Facultad de Ciencias Marinas, UABC uyarbuh@uabc.edu.mx
GRACIAS!