Contrasts in early Miocene subsidence history across Oceanic-West Huasna fault system, northern Santa Maria province, California

Conference · Fri Feb 01 00:00:00 EST 1991 · AAPG Bulletin (American Association of Petroleum Geologists); (United States)

OSTI ID:5170898

Tennyson, M E ^[1]; Keller, M A ^[2]; Filewicz, N V; Thornton, M L.C. ^[3]

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1. Geological Survey, Denver, CO (United States)
2. Geological Survey, Menlo Park, CA (United States)
3. Unocal, Ventura, CA (United States)

Within the Oceanic-West Huasna fault system of western San Luis Obispo County, thick bathyal mudstone records abrupt early Miocene subsidence. Lower Miocene rocks west of the fault, in contrast, suggest a relative high. Between fault splays, {le} 1,800 ft of mudstone (Rincon Formation) contains Saucesian lower bathyal foraminifera and CN2-CN1c ({approximately} 17-21 Ma) nannofossils. The mudstone was deposited on a subsiding erosional surface cut on Great Valley and Franciscan basement overlain locally by late Oligocene rhyodacite (Cambria Felsite), nonmarine conglomerate (Lospe Formation), and nearshore sandstone (Vaqueros Formation). Basinal late early to middle Miocene Obispo and Monterey formations overlie the older mudstone. West of the fault, major subsidence does not conclusively predate {approximately} 17 Ma submarine Obispo tuff. Northeast of Morro Bay, nearshore Vaqueros underlies Obispo or Monterey formations. Northeast of Santa Maria, Franciscan rocks are overlain by thin nonmarine conglomerate, sandstone with upper bathyal Saucesian foraminifera and upper CN2 nannofossils, and Obispo volcanics. Near Cambria, nonmarine conglomerate and Vaqueros sandstone were deposited on the Franciscan between {approximately} 27-27 Ma (Cambria Felsite) and 25 Ma ({sup 87}Sr/{sup 86}Sr on Vaqueros shells); only {approximately}100 ft of basinal mudstone separates Vaqueros from obispo tuff. In the Pismo syncline, the Franciscan was near sea level 25 Ma ({sup 87}Sr/{sup 86}Sr or shells); subsidence to bathyal depths cannot be demonstrated until just before Obispo eruption. Paleobathymetric estimates suggest initiation of at least 6,000 ft of subsidence along the fault system {approximately} 20-21 Ma. The block to the west, in contrast, either stayed high, or subsided but was uplifted and stripped, subsiding again as Obispo eruption began. The authors have not found evidence for major lateral offset on this fault.

• OSTI ID: 5170898
• Report Number(s): CONF-9103128-; CODEN: AABUD
• Journal Information: AAPG Bulletin (American Association of Petroleum Geologists); (United States), Vol. 75:2; Conference: American Association of Petroleum Geologists (AAPG)/Society of Economics, Paleontolgists, and Mineralogists (SEPM)/Society of Exploration Geophysicists (SEG)/Society of Professional Well Log Analysts (SPWLA) Pacific Section annual meeting, Bakersfield, CA (United States), 6-8 Mar 1991; ISSN 0149-1423
• Country of Publication: United States
• Language: English

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58 GEOSCIENCES
CALIFORNIA
SEDIMENTARY BASINS
GEOLOGIC HISTORY
STRATIGRAPHY
BATHYMETRY
CONGLOMERATES
DEPOSITION
GEOLOGIC FAULTS
GEOLOGIC FORMATIONS
MIOCENE EPOCH
SANDSTONES
SHALES
CENOZOIC ERA
DEVELOPED COUNTRIES
GEOLOGIC AGES
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
GEOLOGY
NORTH AMERICA
ROCKS
SEDIMENTARY ROCKS
TERTIARY PERIOD
USA
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