Syn-sedimentary tectonostratigraphic influence and isotopic δ18O and δ13C characterization of the Kimmeridgian Akimpech Formation, Campeche-Chiapas Subbasin (Campeche Sound), offshore Mexico.

Carbonate reservoirs are notoriously heterogeneous, with variability driven by both depositional and diagenetic controls. In such reservoirs, conceptual models play an important role in generating understanding and predictive insights. Yet, predictions are only as good as the conceptual models. This work investigates the structural and stratigraphic controls on the deposition and early- to late-diagenetic evolution of the Late Jurassic (Kimmeridgian) Akimpech Formation in the Campeche-Chiapas Subbasin, offshore Mexico and tests two dominant paradigms.

Name thesis:degree_name

Ph.D.

Discipline thesis:degree_discipline

Geology

Grantor dc:publisher

University of Kansas

Year dc:date.issued

2026

Author dc:creator

• Cuapio-Perez, César Augusto

Advisors dc:contributor.advisor

• Rankey, Eugene C
• González, Luis A

• carbon and oxygen isotopes
• Dolomite reservoir
• Gulf of Mexico
• Jurassic Kimmeridgian
• mixed Carbonates
• Tectonics

Language dc:language.iso

en

Dc Identifier Other

https://www.proquest.com/LegacyDocView/DISSNUM/32703567

OAI identifier oai:identifier

oai:kuscholarworks.ku.edu:1808/39428