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migration into Sespe red beds

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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1947
AAPG Bulletin (1947) 31 (11): 1913–1935.
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1946
AAPG Bulletin (1946) 30 (12): 2089.
...Thomas L. Bailey ABSTRACT The name “Sespe formation” is applied to the non-marine red bed facies of a group of sedimentary rocks up to 7,500 feet thick. They range in age from upper Eocene into lower Miocene in the southern and eastern part of the Ventura basin but are probably confined...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1982
AAPG Bulletin (1982) 66 (7): 805–829.
... and are seismogenic. The Rincon Creek fault dips 35 to 60° south, steepening to nearly vertical at depth, where it apparently passes into bedding within the Sespe Formation. The Rincon Creek fault offsets late Pleistocene marine terraces and is itself deformed by the Red Mountain fault. The Red Mountain fault dips 55...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1947
AAPG Bulletin (1947) 31 (11): 1913–1935.
... the fine sandstones and argillaceous beds are still red. Two or three miles northwest of the Capitan oil field, marine fossils begin to appear in the buff-weathering sandstones near the base of the Sespe and finally, north of Santa Anita Station, which is about 10 miles east-northeast of Pt. Concepcion...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1924
AAPG Bulletin (1924) 8 (6): 789–829.
... .—In the region of South Mountain the Sespe series includes over 6,000 feet of sandstone, clayey sandstone, and shale. This great thickness of beds is a typical “red bed” series, and, from its lithologic character and the lack of remains of marine organisms, it is believed to be of non-marine origin...
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..., bedding characteristics and sedimentary structures ( Table 1 ). Facies A, B, C, and D are the most widespread and are generally present in sequential order as the Sespe Formation is stratigraphically ascended. Facies C makes up the bulk of the Sespe Formation throughout its area of extent, whereas facies...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1993
AAPG Bulletin (1993) 77 (9): 1509–1518.
... anhydrite + 1.125   H 2 O+ HC Figure 3 —Schematic diagram for paired point-count results from oxidized red (stippled) and reduced white (no pattern) areas from single thin sections. Analyses were made for three samples from the Sespe Formation, California, for three different...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1976
AAPG Bulletin (1976) 60 (1): 65–86.
... is similar ( Yeats et al, 1974 ), consisting of red, maroon, and gray sandstone and cobble conglomerate, with green and maroon siltstone and mudstone. In the eastern Santa Monica Mountains, the typical Sespered beds” are absent, and may be represented by several hundred feet of brown cobble conglomerate...
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Journal Article
Journal: Geosphere
Published: 15 October 2020
Geosphere (2020) 16 (6): 1425–1456.
.... 20 Ma) components of the Sespe Formation include a diverse population of white, black, red, and green pebbles and cobbles that include metaquartzite and silica-cemented orthoquartzite that range in composition from quartz arenite to arkose. Figure 1 shows potential source regions...
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Journal Article
Journal: Geosphere
Published: 16 October 2019
Geosphere (2019) 15 (6): 1973–1998.
... localities (black dots) with Sespe depositional ages, including: 1—View Lane Drive locality in Simi Valley; 2—Piuma Road and Scheuren Road localities in the Santa Monica Mountains; and 3—Red Rock Trail in Limestone Canyon Park and Santiago Canyon Road localities in the Santa Ana Mountains ( Tables 2 and 3...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2000
GSA Bulletin (2000) 112 (11): 1635–1649.
.../2) and orangish-red (10R3/4–10R4/2) types are also conspicuous. The middle part of the black and green quartzite clast assemblage corresponds to a stratigraphic interval in which all Sespe conglomerate clasts coarsen upward into boulder conglomerate. Essentially all quartzite clasts are extremely...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1982
AAPG Bulletin (1982) 66 (10): 1514–1534.
.... The upper Matilija Sandstone consists of shallow-marine cross-bedded sandstone, red beds, and carbonate-evaporite-lignite sequences which overlie the turbidites. Deposition of the Matilija Sandstone was terminated by a rapid basin deepening event which culminated in deposition of basin plain, slope...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1991
AAPG Bulletin (1991) 75 (8): 1353–1373.
... Cayetano fault ( Figure 2 ) and at its type section in a tributary to Sespe Creek ( Figure 1 ) ( Kerr and Schenk, 1928 ). The upper Eocene and Oligocene Sespe Formation ( Kew, 1924 ) is cut by the San Cayetano fault, so that a complete section is not found at the surface in the study area. To the west...
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Series: GSA Special Papers
Published: 28 December 2018
DOI: 10.1130/2018.2540(20)
EISBN: 9780813795409
... al. (2004) . Vertical lines indicate lack of stratigraphic record, due to either nondeposition or erosion. L—Late; M—Middle; E—Early. Previous Work The Sespe Formation was originally defined as a series of red beds by Watts (1897) at the Sespe Creek type locality north of the city...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1994
AAPG Bulletin (1994) 78 (7): 1040–1074.
... the Aliso Canyon and Placerita oil fields, upper Miocene marine strata are underlain unconformably by nonmarine beds known only from the subsurface; these rest on marine Eocene rocks ( Winterer and Durham, 1962 ; Nelligan, 1978 ) (for map extent, see Figure 3 ). The sequence consists of gray, red, green...
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Series: Guidebook
Published: 01 January 1996
DOI: 10.32375/1996-GB73.10
EISBN: 9781732014848
... of Ojai, the low foothills of the Santa Ynez Mountains are underlain by red beds of the Sespe Formation. On the west side of the highway, these beds extend over the higher hills up to the skyline. The white outcrops at and near the skyline are beds of the Coldwater Formation. Quaternary terrace gravels...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1951
AAPG Bulletin (1951) 35 (12): 2542–2560.
... Sespe section is exposed on Red Mountain which lies north of the San Miguelito field. The areal geology of this region was described in 1942 by Wm. C. Putnam. 4 Good exposures of Miocene rocks occur around the flanks of the Red Mountain anticline. The Vaqueros is approximately 300 feet thick...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1996
AAPG Bulletin (1996) 80 (5): 770–779.
... at an angular unconformity ( Figure 5B , C), along which there is southerly truncation of underlying Miocene beds by progressively onlapping and thinning Pliocene beds (Tpp) until the Pliocene eventually rests on the Oligocene Sespe (Os) Formation ( Figure 5C ). This is not the expected stratigraphic geometry...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2000
GSA Bulletin (2000) 112 (7): 1080–1090.
... in the west to 8 km in the east ( Figs. 2 and 3 ; Yeats, 1988 ). The western portion of the Ventura basin underlies the northern Santa Barbara Channel (Fig. 1) . In the east (onshore), the basin is bordered by the north-dipping San Cayetano and Red Mountain reverse faults on the north and by the south...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1973
AAPG Bulletin (1973) 57 (11): 2217–2244.
... at room temperature. Thus, Moulton concluded that it may not be the migrating oil but the H 2 S in associated formation waters that bleaches red beds. Possibly the formation waters in the Lyons Sandstone near the center of the basin were highly alkaline because the formation pinches out...
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