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Santa Fe-Coyote Fault

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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1973
AAPG Bulletin (1973) 57 (4): 789-790.
... earthquake occurred in 1929 along the Norwalk fault 6 mi south of the Whittier fault. Analysis of precise level lines run by the Los Angeles County Engineers since 1951 indicates that the Puente and Montebello Hills area and the Santa Fe Springs-Coyote Hills trend are rising at a rate of 0.01 to 0.04 ft/year...
Series: GSA Special Papers
Published: 01 January 1994
DOI: 10.1130/SPE291-p113
...-Placitas faults). In the south, it thickens westward toward the Santa Fe-Coyote master faults along the southwestern margin of the basin. As a result, depositional rates of the Santa Fe were rapid on the structurally deep, master-fault sides of the basin in the northeast and southwest and relatively slow...
Journal Article
Published: 01 February 2008
Bulletin of the Seismological Society of America (2008) 98 (1): 106-123.
... basin, California. The modeled uplift matches well the geologic pattern of uplift associated with the Santa Fe Springs and Coyote Hills segments of the Puente Hills thrust fault but does not match structures to the west of the San Gabriel River. To better match the geologic patterns in this area...
FIGURES | View All (9)
Journal Article
Journal: Geosphere
Published: 01 October 2013
Geosphere (2013) 9 (5): 1125-1146.
...– or northeast-trending valleys in granitic basement, but have no corroborating evidence in the form of offset of Cenozoic strata (e.g., see Silver King fault, Fish Valley fault, and Coyote Valley fault; Fig. 2 ; first mapped by Slemmons, 1953 ). Middle Miocene andesitic volcanic and volcaniclastic rocks...
FIGURES | View All (17)
Journal Article
Journal: Geosphere
Published: 01 June 2013
Geosphere (2013) 9 (3): 614-646.
... Ma) to east (5–2 Ma) pattern that reflects the timing of motion on faults. The new ages, coupled with detailed mapping of both volcanic rocks and the Santa Fe Group, document significant pulses of faulting, erosion, and deposition during middle Miocene time and during late Miocene time across...
FIGURES | View All (15)
Journal Article
Journal: Geosphere
Published: 01 April 2014
Geosphere (2014) 10 (2): 401-423.
... is located on the eastern side of the Lucero uplift along a reactivated reverse fault called the Comanche fault that, along with the Cenozoic Santa Fe normal fault, separates Precambrian and older Paleozoic carbonates from younger Cenozoic rocks ( Figs. 2 and 4B ; Barker et al., 1996 ). Travertine...
FIGURES | View All (12)
Journal Article
Journal: Geosphere
Published: 01 April 2016
Geosphere (2016) 12 (2): 366-376.
... (diagonal lines below wells). The Santa Clara Valley is between the Santa Cruz Mountains and the Diablo Range in the California Coast Ranges, southeast of San Francisco Bay ( Fig. 1 ). The San Andreas fault cuts through the Santa Cruz Mountains south and west of the valley, and the Hayward...
FIGURES | View All (11)
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1948
AAPG Bulletin (1948) 32 (1): 109-125.
... of 5,000 feet below sea-level. FIG. 2 GENERALIZED FAULT PATTERN & STRATIGRAPHIC CONTACTS 5000 FT. BELOW SEA LEVEL LOS ANGELES BASIN CALIFORNIA Figure 1 shows the principal structural provinces in the vicinity of the Los Angeles Basin. This Basin is bounded on the north by the Santa...
FIGURES | View All (4)
Journal Article
Published: 01 April 2004
Bulletin of the Seismological Society of America (2004) 94 (2): 493-505.
... west to east, these segments are the Los Angeles, Santa Fe Springs, and Coyote Hills thrust faults (Figs. 1 and 3 ). The geometry and slip rates of all three segments of the PHT have been inferred from seismic reflection images of fold growth structures associated with the upper fault tips ( Shaw...
FIGURES | View All (7)
Journal Article
Published: 01 August 2005
Bulletin of the Seismological Society of America (2005) 95 (4): 1263-1275.
... faults include the West Sierra Madre (WSM), East Sierra Madre (ESM), Verdugo (VF), San Gabriel (SG), Clamshell-Sawpit (CS), Cucamonga (CU), San Jose (SJ), Northridge (NF), Los Angeles (LA), Santa Fe Springs (SFS), Coyote Hills (CH), Whittier (WF), Santa Monica (SM), Hollywood (HW), Raymond (RF), San...
FIGURES | View All (5)
Journal Article
Journal: Geology
Published: 01 March 2017
Geology (2017) 45 (3): 227-230.
..., the Coyote Hills, Santa Fe Springs, and Los Angeles ( Fig. 1A ). The tips of these faults are overlain by a series of east-west–trending, en echelon anticlines ( Shaw et al., 2002 ; Leon et al., 2007 ). Using earthquake magnitude-scaling relationships for thrust faults ( Wells and Coppersmith, 1994...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 September 2004
GSA Bulletin (2004) 116 (9-10): 1143-1157.
...-field data. Profile B–B′ (Fig. 5) crosses the Peninsular Ranges batholith boundary near its intersection with the San Jacinto fault zone, crossing the Lakeview Mountains pluton. The southernmost section cutting the Peninsular Ranges batholith, the Coyote Creek section, consists primarily...
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Journal Article
Published: 01 March 2002
Bulletin of the Seismological Society of America (2002) 92 (2): 695-710.
... A HCP 33.676 – 116.68 Hurkey Creek Park USGS B ISD 35.65 – 118.47 Isabella Dam (Aux abut) ACOE A JOS 33.944 – 118.087 Santa Fe Springs–E Joslin USC B KOD 37.729 – 121.928 San Ramon–Eastman Kodak CDMG B L04 34.642 – 118.481 Lake Hughes #4 USGS A L09 34.610...
FIGURES | View All (6)
Journal Article
Journal: GSA Bulletin
Published: 01 September 2004
GSA Bulletin (2004) 116 (9-10): 1158-1182.
... with exposures in the Santa Ana Mountains and along the Elsinore fault. Nonmarine fluvial strata in the Santa Ana Mountains and in the subsurface of the Puente Hills, correlated to the Eocene–Oligocene Sespe Formation of the Ventura Basin, were mapped as “Sespe-Vaqueros” by Schoellhamer et al. (1981...
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Image
Comparison of modeled reverse-slip distribution across PHT <b>faults</b> to rates ...
Published: 01 April 2004
Figure 5. Comparison of modeled reverse-slip distribution across PHT faults to rates inferred from structural relief assuming a fault dip of 27° ( Shaw et al. , 2002 ). Reverse-slip rates for Los Angeles (LA), Santa Fe Springs (SFS), and Coyote Hills (CH) faults are represented by gray dotted
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1930
AAPG Bulletin (1930) 14 (8): 997-1011.
... of the isothermal surface from the center to the boundaries of the basin, and the agreement of the isothermal elevations in the West Coyote field with the surface established in the Santa Fe Springs field. Evidently these results do not establish any certain correlation between geothermal variations...
FIGURES | View All (5)
Journal Article
Journal: Geosphere
Published: 01 February 2016
Geosphere (2016) 12 (1): 237-263.
... regard porphyry molybdenum mineralization at Spruce Mountain as having formed in the late Eocene, ca. 38 Ma. TABLE 2. FAULTS AND FAULT SETS AT SPRUCE MOUNTAIN In the northwestern part of the Spruce Mountain district, six holes drilled by Santa Fe Mining in the mid-1980s intersected...
FIGURES | View All (10)
Series: Geological Society, London, Special Publications
Published: 02 December 2019
DOI: 10.1144/SP488-2019-272
EISBN: 9781786204639
... to the north by the Santa Monica Fault and to the east by the San Andreas Fault ( Fig. 1b ). The Los Angeles Basin has evolved within the framework of this right-lateral transform fault system, which separates the North American Plate to the east from the Pacific Plate to the west. Many of the basin-fill units...
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Image
Map view projection of three-dimensional geometry of modeled <b>faults</b> include...
Published: 01 April 2004
Figure 3. Map view projection of three-dimensional geometry of modeled faults includes Los Angeles (LA), Santa Fe Springs (SFS), Coyote Hills (CH), Whittier (WF), Santa Monica (SM), Hollywood (HW), Raymond (RF), San Vicente (SV), Las Cienagas (LC), Alhambra (AF), Richfield (RH), Peralta Hills (PH
Journal Article
Published: 01 December 2002
Bulletin of the Seismological Society of America (2002) 92 (8): 2946-2960.
... , 6 ). Similar to the Santa Fe Springs structure, the Coyote Hills anticline is a broad, open fold bounded on its southern margin by a discrete forelimb kink band (aa′) that contains parallel, south-dipping (15°-30°) Pliocene strata. The fault extends upward to the base of this kink band, which...
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