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Santa Barbara Belt

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Journal Article
Journal: GSA Bulletin
Published: 01 January 2014
GSA Bulletin (2014) 126 (1-2): 219–233.
.... The pattern and elevation of shoreline angles on active folds provide information about rates of uplift and fold growth, which is important for defining tectonic models. A particularly impressive succession of marine terraces are developed across the Santa Barbara fold belt (SBFB) in southern California...
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First thumbnail for: Tectonic geomorphology of marine terraces: <span c...
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Map of the eastern Santa Barbara fold belt from Santa Barbara eastward to Summerland. Uplifted marine terraces and the associated paleo-shoreline are shown. The Mission Ridge (MsR), the Fernald Point (FP), the Arroyo Parida (AP), the Santa Barbara Cemetery (SBC), and the Ortega Hill (OH) faults are shown.
Published: 01 January 2014
Figure 10. Map of the eastern Santa Barbara fold belt from Santa Barbara eastward to Summerland. Uplifted marine terraces and the associated paleo-shoreline are shown. The Mission Ridge (MsR), the Fernald Point (FP), the Arroyo Parida (AP), the Santa Barbara Cemetery (SBC), and the Ortega Hill
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Onshore Santa Barbara fold belt showing south-dipping reverse faults, some of which are blind, with associated north-verging, hanging-wall anticlines and footwall synclines. The marine terrace landforms are preserved on anticlinal folds formed as the result of blind reverse and thrust faulting. The Mission Ridge fault system is subdivided into the More Ranch (MrR), the Mission Ridge (MsR), and the Arroyo Parida (AP) segments. Additional onshore reverse faults include the Dos Pueblos (DP), the Carneros (CF), the San Jose (SJ), the San Pedro (SP), the Lavigia (LF), the Mesa (MF), the Santa Barbara Cemetery (SBC), the Ortega Hill (OH), and the Fernald Point (FP) faults. UCSB—University of California–Santa Barbara.
Published: 01 January 2014
Figure 1. Onshore Santa Barbara fold belt showing south-dipping reverse faults, some of which are blind, with associated north-verging, hanging-wall anticlines and footwall synclines. The marine terrace landforms are preserved on anticlinal folds formed as the result of blind reverse and thrust
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Published: 01 January 2014
TABLE 1. NUMERICAL DATES FOR MARINE TERRACE DEPOSITS IN THE SANTA BARBARA FOLD BELT
Journal Article
Journal: GSA Bulletin
Published: 01 May 1994
GSA Bulletin (1994) 106 (5): 607–626.
... Ridge and Blue Bottle trends, which overlie active blind-thrust faults in the eastern Santa Barbara Channel. These folds and their causative faults are interpreted using fault-bend fold theory and are represented in balanced models and cross sections that integrate surface and subsurface data...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1984
AAPG Bulletin (1984) 68 (4): 467.
...James K. Crouch; Steve Bachman Abstract High-resolution, 36-fold seismic reflection data with penetration to 3 sec have been collected recently in the northeastern offshore Santa Maria basin, the northern Santa Barbara Channel, and off Point Conception, California. These profiles reveal major east...
Journal Article
Journal: Geosphere
Published: 01 December 2013
Geosphere (2013) 9 (6): 1766–1782.
... Cenozoic thrust belt with predominantly west-vergent structures in Argentina that transition northward into a bivergent system in Bolivia; and (3) the Santa Bárbara Ranges, a region near the modern deformation front that consists of mainly east-dipping reverse faults, transitioning along strike northward...
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First thumbnail for: Influence of pre-Andean crustal structure on Cenoz...
Second thumbnail for: Influence of pre-Andean crustal structure on Cenoz...
Third thumbnail for: Influence of pre-Andean crustal structure on Cenoz...
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 26 September 2020
Lithosphere (2020) 2020 (1): 8888588.
... by the Subandean foreland fold-and-thrust belt of Bolivia and north-western Argentina, and the broken foreland of the north-western Argentinean Santa Bárbara and Sierras Pampeanas uplifts (Figure 1 ). The Santa Bárbara morphotectonic province is a seismically active low-strain region [ 8 ], characterized...
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First thumbnail for: Neotectonic Activity in the Low-Strain Broken Fore...
Second thumbnail for: Neotectonic Activity in the Low-Strain Broken Fore...
Third thumbnail for: Neotectonic Activity in the Low-Strain Broken Fore...
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 04 November 2019
Lithosphere (2019) 11 (6): 868–883.
.... 1488 – 1497 , https://doi.org/10.1029/94TC02020 . Gurrola , L.D. , Keller , E.A. , Chen , J.H. , Owen , L. , and, Spencer , J.Q. , 2014 , Tectonic geomorphology of marine terraces; Santa Barbara fold belt, California : Geological Society of America Bulletin , v. 126 , p...
FIGURES
First thumbnail for: Structural modeling of the Western Transverse Rang...
Second thumbnail for: Structural modeling of the Western Transverse Rang...
Third thumbnail for: Structural modeling of the Western Transverse Rang...
Journal Article
Published: 01 February 2013
Italian Journal of Geosciences (2013) 132 (1): 54–80.
...-track data along both the Pratomagno and Chianti ridges. Shortening suffered by basin deposits is clearly manifested by the outcrop-scale reverse faults and thrust-related folds affecting the Late Pliocene sediments (Castelnuovo dei Sabbioni Synthem), which are well exposed in the Santa Barbara mine...
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First thumbnail for: Compression-to-extension record in the Late Plioce...
Second thumbnail for: Compression-to-extension record in the Late Plioce...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2000
GSA Bulletin (2000) 112 (7): 1080–1090.
... thrust sheet. Similarly, beyond the well-studied onshore fault, a kinematically continuous offshore Oak Ridge–Mid-Channel left-oblique fault system is interpreted to continue at least an additional 100 km westward beneath the Santa Barbara Channel. The use of geological strata as crustal deformation...
FIGURES
First thumbnail for: Map restoration of folded and faulted late Cenozoi...
Second thumbnail for: Map restoration of folded and faulted late Cenozoi...
Third thumbnail for: Map restoration of folded and faulted late Cenozoi...
Journal Article
Published: 01 March 1982
Bulletin of Canadian Petroleum Geology (1982) 30 (1): 1–8.
... to the Late Cenozoic Ventura Basin and Santa Barbara Channel of California and to the Early Paleozoic South Mayo Trough of Ireland. 1 Department of Geological Sciences, Cornell University, Ithaca, New York 14853. Copyright © 1982, The Canadian Society of Petroleum Geologists 1982 BULLETIN...
Journal Article
Journal: Geology
Published: 01 September 1977
Geology (1977) 5 (9): 557–562.
... contain Early or Middle Jurassic radiolarians. The Jurassic radiolarian fauna from the North Fork terrane is similar to a fauna contained in Franciscan chert near Santa Barbara in southern California. The change in age assignment of the dominant rocks of these terranes, based on this new radiolarian data...
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Published: 01 January 2014
TABLE 2. ESTIMATED UPLIFT RATES OF FIRST EMERGENT TERRACES OF THE SANTA BARBARA FOLD BELT
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Published: 01 January 2014
TABLE 3. LIST OF MARINE TERRACE FLIGHTS, FROM WEST TO EAST, IN THE SANTA BARBARA FOLD BELT
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(a) Spatial location of the Brasília Belt within Brazil. (b) Simplified geological map of the Anicuns region, highlighting the Anápolis–Itauçu Complex and Arenópolis Arc (Sanclerlândia and Turvânia blocks, Anicuns–Itaberaí Sequence), which host multiple mafic–ultramafic intrusions: (1–2) Mangabal Complex, (3) Americano do Brasil Complex, (4) Água Fria, (5) Adelândia, (6) Fronteira Norte, (7) Córrego Seco, (8) Águas Claras, (9) Capelinha, (10) Taquaral, (11) Santa Rosa, (12) Damolândia, (13) Santa Bárbara, (14) Goianira-Trindade, (15) Palmeiras. (c) Simplified geological map of the Mangabal Complex. (d) Simplified geological map of the Americano do Brasil Complex.
Published: 24 June 2025
–2) Mangabal Complex, (3) Americano do Brasil Complex, (4) Água Fria, (5) Adelândia, (6) Fronteira Norte, (7) Córrego Seco, (8) Águas Claras, (9) Capelinha, (10) Taquaral, (11) Santa Rosa, (12) Damolândia, (13) Santa Bárbara, (14) Goianira-Trindade, (15) Palmeiras. ( c ) Simplified geological map
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A: Morphotectonic map of southern Central Andes showing mean annual rainfall derived from National Aeronautics and Space Administration Tropical Rainfall Measurement Mission (after Strecker et al., 2007) and main moisture transport (white arrow) to the study area (black box). EC—Eastern Cordillera, SFTB—Subandean fold-thrust belt; SBS—Santa Barbara system. B: Digital elevation model with sample locations of volcanic ashes (white) and modern water (black) in Humahuaca catchment (dashed line).
Published: 01 August 2014
—Eastern Cordillera, SFTB—Subandean fold-thrust belt; SBS—Santa Barbara system. B: Digital elevation model with sample locations of volcanic ashes (white) and modern water (black) in Humahuaca catchment (dashed line).
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Along-strike variations in stratigraphy and previous estimates of the magnitude of retroarc shortening. (A) N-S stratigraphic section across retroarc thrust belt, modified from Allmendinger and Gubbels (1996). Mz—Mesozoic; Carb.—Carboniferous; Ordo—Ordovician. (B) Predicted (assuming an initially 40-km-thick crust and local isostatic compensation; Isacks, 1988; Kley and Monaldi, 1998) versus observed (Oncken et al., 2006) magnitudes of shortening in retroarc thrust belt of southern Central Andes. A revised estimate of 142 km of shortening accommodated by the Eastern Cordillera at ∼24.75°S is the sum of current results and existing estimates for the Puna Plateau (Coutand et al., 2001) and Santa Bárbara Ranges (Kley and Monaldi, 2002).
Published: 01 December 2013
at ∼24.75°S is the sum of current results and existing estimates for the Puna Plateau ( Coutand et al., 2001 ) and Santa Bárbara Ranges ( Kley and Monaldi, 2002 ).
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A: Rainfall distribution and morphotectonic provinces, Central Andes, highlighting the impact of high topography on easterly moisture transport. SFTB—Subandean foreland fold-and-thrust belt; EC—Eastern Cordillera; SBS—Santa Bárbara System. B: Topographic overview showing location of Humahuaca Basin to the east of the Puna Plateau margin (white line) in northwest Argentina. Black lines delineate catchments discussed in the text. *Estimates of modern catchment-wide denudation rates in mm/yr (Bookhagen and Strecker, 2012; Schildgen et al., 2016). C: Shaded relief map showing distribution of late Miocene–Pliocene strata in the Humahuaca Basin with sample locations color-coded by depositional age.
Published: 26 February 2019
Figure 1. A: Rainfall distribution and morphotectonic provinces, Central Andes, highlighting the impact of high topography on easterly moisture transport. SFTB—Subandean foreland fold-and-thrust belt; EC—Eastern Cordillera; SBS—Santa Bárbara System. B: Topographic overview showing location
Journal Article
Journal: GSA Bulletin
Published: 01 July 2000
GSA Bulletin (2000) 112 (7): 1067–1079.
... the Santa Monica Mountains through the southern Santa Barbara Channel. The north-dipping backlimb of this anticline is 20–30 km wide and 220 km long; its presence suggests a very large north-dipping thrust that could generate very large earthquakes. The slip rate for this fault, however, is substantially...
FIGURES
First thumbnail for: Listric thrusts in the western Transverse Ranges, ...
Second thumbnail for: Listric thrusts in the western Transverse Ranges, ...
Third thumbnail for: Listric thrusts in the western Transverse Ranges, ...