Quick Search:    advanced search

GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Citation Map Services Email this article to a friend Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via Google Scholar Google Scholar Articles by Vermeesch, P. Articles by McWilliams, M. O. Search for Related Content GeoRef GeoRef Citation

Multimethod detrital thermochronology of the Great Valley Group near New Idria, California

Pieter Vermeesch^,1, Donald D. Miller^,2, Stephan A. Graham^,3, Johan De Grave^#,4 and Michael O. McWilliams^,5

¹ Department of Geological and Environmental Sciences, Stanford University, Braun Hall, room 320, 450 Serra Mall, Stanford, California 94305-2115, USA
² Aera Energy, LLC, P.O. Box 11164, Bakersfield, California 93389-1164, USA
³ Department of Geological and Environmental Sciences, Stanford University, Braun Hall, room 320, 450 Serra Mall, Stanford, California 94305-2115, USA
⁴ Geological Institute, University of Gent, Krijgslaan 281, B-9000 Gent, Belgium
⁵ Department of Geological and Environmental Sciences, Stanford University, Braun Hall, room 320, 450 Serra Mall, Stanford, California 94305-2115, USA

The simultaneous use of several thermochronological methods on replicate sedimentary rock samples can reveal their pre- and postdepositional history. Single grain U/Pb dating of zircon, zircon and apatite fission track dating, and vitrinite reflectance measurements were performed on Cretaceous through Miocene sedimentary rocks of the Great Valley Group and the Temblor Formation near Coalinga and New Idria, California. The data show that the Sierra Nevada was exhumed and cooled at 0.5–1 km/m.y. or 20 °C/m.y. during the Cretaceous. After deposition in the Great Valley forearc basin, Sierra Nevada erosional products were buried at great depth under low thermal gradients. At ca. 12–14 Ma, northward progression of the Mendocino triple junction triggered folding on the eastern flanks of the California Coast Ranges and rapid exhumation of the New Idria serpentinite diapir. This middle Miocene event caused the deposition of spectacular deposits of sedimentary serpentinite (Big Blue Formation). The rapid rise of the hot serpentinite body created a thermal pulse that may have provided the enigmatic heat source for oil fields in the shallow Vallecitos syncline, a few kilometers north of New Idria.

Key Words: detrital thermochronology • fission track • Great Valley Group • serpentinite • Sierra Nevada • exhumation

This article has been cited by other articles:

				T. Tsujimori, J. G. Liou, and R. G. Coleman Finding of high-grade tectonic blocks from the New Idria serpentinite body, Diablo Range, California: Petrologic constraints on the tectonic evolution of an active serpentinite diapir Geological Society of America Special Papers, January 1, 2007; 419(0): 67 - 80. [Abstract] [Full Text] [PDF]

				I. S.E. Carmichael, R. A. Lange, C. M. Hall, and P. R. Renne Faulted and tilted Pliocene olivine-tholeiite lavas near Alturas, NE California, and their bearing on the uplift of the Warner Range Geological Society of America Bulletin, September 1, 2006; 118(9-10): 1196 - 1211. [Abstract] [Full Text] [PDF]