Geological Studies in eastern Venezuela and Trinidad from Cretaceous passive margin to Neogene transpressional thrust belt
Abstract
Sedimentological and structural analyses of Trinidad's Northern and Central ranges and Venezuela's Serrania del Interior have led to new interpretations of northeastern. South America's tectonic evolution within the Southern Caribbean Plate Boundary Zone. Medial ( ) Jurassic through early Cenozoic passive margin sediments make up the majority of these areas and were deposited somewhat to the WNW (between 80 and 130 km for Northern Range of Trinidad) of their present positions prior to structural shortening. Neogene southeastward displacement of Jurassic-Cretaceous passive slope and rise sediments (Northern Range) drove propagation of thrusts southward into the Serrania and Central ranges. Displacements were driven by migration of the Caribbean Plate relative to South America. Thus, the Serrania and Central ranges are the western hemisphere's only exposed Mesozoic-Cenozoic passive Atlantic margin stratigraphic section. As such, they provide a Cretaceous-Paleogene record of passive margin sedimentation at a thermally subsiding margin where the complicating effects of tectonism are absent. This makes these sections especially suited for studies of eustatic sea level behavior. Preliminary assessments are shown which suggest that sea level changes for Cretaceous to Paleogene time are not as pronounced as the frequent large and rapid sea level falls and rises that are promoted bymore »
- Authors:
-
- Dartmouth Coll., Hanover, NH (United States)
- Publication Date:
- OSTI Identifier:
- 5904586
- Report Number(s):
- CONF-910403-
Journal ID: ISSN 0149-1423; CODEN: AABUD
- Resource Type:
- Conference
- Journal Name:
- AAPG Bulletin (American Association of Petroleum Geologists); (United States)
- Additional Journal Information:
- Journal Volume: 75:3; Conference: Annual meeting of the American Association of Petroleum Geologists (AAPG), Dallas, TX (United States), 7-10 Apr 1991; Journal ID: ISSN 0149-1423
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; PLATE TECTONICS; GEOLOGIC MODELS; TRINIDAD AND TOBAGO; VENEZUELA; CRETACEOUS PERIOD; GEOLOGIC FAULTS; GEOLOGIC HISTORY; JURASSIC PERIOD; SEA LEVEL; DEVELOPING COUNTRIES; GEOLOGIC AGES; GEOLOGIC FRACTURES; GEOLOGIC STRUCTURES; ISLANDS; LATIN AMERICA; LESSER ANTILLES; LEVELS; MESOZOIC ERA; SOUTH AMERICA; TECTONICS; WEST INDIES; 580000* - Geosciences
Citation Formats
Algar, S T, Erikson, J E, and Pindell, J L. Geological Studies in eastern Venezuela and Trinidad from Cretaceous passive margin to Neogene transpressional thrust belt. United States: N. p., 1991.
Web.
Algar, S T, Erikson, J E, & Pindell, J L. Geological Studies in eastern Venezuela and Trinidad from Cretaceous passive margin to Neogene transpressional thrust belt. United States.
Algar, S T, Erikson, J E, and Pindell, J L. 1991.
"Geological Studies in eastern Venezuela and Trinidad from Cretaceous passive margin to Neogene transpressional thrust belt". United States.
@article{osti_5904586,
title = {Geological Studies in eastern Venezuela and Trinidad from Cretaceous passive margin to Neogene transpressional thrust belt},
author = {Algar, S T and Erikson, J E and Pindell, J L},
abstractNote = {Sedimentological and structural analyses of Trinidad's Northern and Central ranges and Venezuela's Serrania del Interior have led to new interpretations of northeastern. South America's tectonic evolution within the Southern Caribbean Plate Boundary Zone. Medial ( ) Jurassic through early Cenozoic passive margin sediments make up the majority of these areas and were deposited somewhat to the WNW (between 80 and 130 km for Northern Range of Trinidad) of their present positions prior to structural shortening. Neogene southeastward displacement of Jurassic-Cretaceous passive slope and rise sediments (Northern Range) drove propagation of thrusts southward into the Serrania and Central ranges. Displacements were driven by migration of the Caribbean Plate relative to South America. Thus, the Serrania and Central ranges are the western hemisphere's only exposed Mesozoic-Cenozoic passive Atlantic margin stratigraphic section. As such, they provide a Cretaceous-Paleogene record of passive margin sedimentation at a thermally subsiding margin where the complicating effects of tectonism are absent. This makes these sections especially suited for studies of eustatic sea level behavior. Preliminary assessments are shown which suggest that sea level changes for Cretaceous to Paleogene time are not as pronounced as the frequent large and rapid sea level falls and rises that are promoted by some.},
doi = {},
url = {https://www.osti.gov/biblio/5904586},
journal = {AAPG Bulletin (American Association of Petroleum Geologists); (United States)},
issn = {0149-1423},
number = ,
volume = 75:3,
place = {United States},
year = {Fri Mar 01 00:00:00 EST 1991},
month = {Fri Mar 01 00:00:00 EST 1991}
}