Relationship between relative sea level fluctuations and petrologic variation in forearc basin sedimentary rocks of Upper Cretaceous Rosario Formation at San Carlos, Baja California del Norte, Mexico
Conference
·
· AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
OSTI ID:6070754
Petrographic study of a well-exposed submarine canyon fill sequence indicates that petrologic variation corresponds to changes in relative sea level. These changes are recorded as textural variation in the canyon fill: a basal coarse-grained unit capped by a middle fine-grained unit records a rise in sea level, and an upper coarse-grained unit records a temporary fall in sea level. These sea level fluctuations do not correlate with published eustatic sea level curves, although the temporary fall may be recorded on a regional (San Diego to San Carlos, 400 km) scale. Sandstone samples from the lower and upper coarse-grained units contain higher concentrations of volcanic rock fragments and plagioclase than the middle fine-grained unit, whereas the middle fine-grained unit contains higher concentrations of quartz and K-feldspar. Fluctuations in relative sea level may have been controlled by tectonic or magmatic events: (1) a tectonically controlled rise in relative sea level could have resulted in longer residence tie of the sediment in a nearshore environment, causing increased mechanical and chemical weathering of the least-resistant grains (i.e., plagioclase and volcanic fragments) relative to quartz and K-feldspar; or (2) a temporary lull in volcanism could have resulted in increased dissection of the arc and decreased sediment input due to lowered base level within the arc, resulting in a marine transgression and an increase in the concentration of quartz and K-feldspar in the sediment. The lack of significant alteration of the feldspar grains in the fine-grained unit relative to the coarse-grained units may favor the second hypothesis.
- Research Organization:
- Univ. of California, Santa Barbara
- OSTI ID:
- 6070754
- Report Number(s):
- CONF-870606-
- Conference Information:
- Journal Name: AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States) Journal Volume: 71:5
- Country of Publication:
- United States
- Language:
- English
Similar Records
Sedimentologic evolution of a submarine canyon in a forearc basin, Upper Cretaceous Rosario Formation, San Carlos, Mexico
Petrology and provenance of modern sands from Cascade Range Forearc and Canadian Rocky Mountain fold-thrust belt
Submarine canyon in a forearc basin, Upper Cretaceous Rosario Group, Baja California, Mexico
Journal Article
·
Wed Jun 01 00:00:00 EDT 1988
· AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
·
OSTI ID:6023607
Petrology and provenance of modern sands from Cascade Range Forearc and Canadian Rocky Mountain fold-thrust belt
Conference
·
Fri May 01 00:00:00 EDT 1987
· AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
·
OSTI ID:6220143
Submarine canyon in a forearc basin, Upper Cretaceous Rosario Group, Baja California, Mexico
Conference
·
Mon Mar 31 23:00:00 EST 1986
· Am. Assoc. Pet. Geol., Bull.; (United States)
·
OSTI ID:6987528
Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
CRETACEOUS PERIOD
DEVELOPING COUNTRIES
FELDSPARS
GEOLOGIC AGES
GEOLOGIC FORMATIONS
GEOLOGIC STRUCTURES
GEOLOGY
LATIN AMERICA
MESOZOIC ERA
MEXICO
MINERALS
NORTH AMERICA
ROCKS
SANDSTONES
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
STRATIGRAPHY
TECTONICS
020200* -- Petroleum-- Reserves
Geology
& Exploration
CRETACEOUS PERIOD
DEVELOPING COUNTRIES
FELDSPARS
GEOLOGIC AGES
GEOLOGIC FORMATIONS
GEOLOGIC STRUCTURES
GEOLOGY
LATIN AMERICA
MESOZOIC ERA
MEXICO
MINERALS
NORTH AMERICA
ROCKS
SANDSTONES
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
STRATIGRAPHY
TECTONICS