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Bouse Hills

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Geologic map of the northern Plomosa Mountains and western <b>Bouse</b> <b>Hills</b>. Poi...
Published: 18 October 2018
Figure 3. Geologic map of the northern Plomosa Mountains and western Bouse Hills. Points A, B, and C (in red) are used as markers for calculation of total extension. Simplified from Spencer and Reynolds (1990a) , Spencer et al. (2015) , and Strickland et al. (2017b) . See Figure 2
Journal Article
Journal: Geosphere
Published: 01 June 2014
Geosphere (2014) 10 (3): 462–475.
...David M. Miller; Robert E. Reynolds; Jordon E. Bright; Scott W. Starratt Abstract Limestone beds underlain and overlain by alluvial fan conglomerate near Amboy, California, are very similar in many respects to parts of the Bouse Formation, suggesting that an arm of the Pliocene Bouse water body...
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Journal Article
Journal: Geosphere
Published: 01 June 2013
Geosphere (2013) 9 (3): 444–459.
... Wind Caves Member within a reverse-polarity period dated as 4.89–4.98 Ma, slightly inconsistent with indicated arrival of the Colorado River and deposition of the Bouse Formation and the 4.83 Ma Lawlor Tuff. The Mud Hills Member is identified as containing the Nunivak, Sidufjall, and upper Thvera...
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Journal Article
Journal: Geosphere
Published: 20 December 2019
Geosphere (2020) 16 (1): 111–135.
... corridor (southwestern USA) during and after the latest Miocene Epoch, postdating large-magnitude extension and metamorphic core complex formation. Geometric and kinematic data collected on faults in key geologic units constrain the timing of deformation in relation to the age of the Bouse Formation...
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Journal Article
Journal: Geosphere
Published: 08 June 2018
Geosphere (2018) 14 (4): 1875–1911.
...Jordon Bright; Andrew S. Cohen; David L. Dettman; Philip A. Pearthree Abstract Uncertainty over the depositional environment of the late Miocene and early Pliocene Bouse Formation hinders our understanding the evolution of the lower Colorado River corridor. Competing marine and lacustrine models...
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Journal Article
Journal: Geosphere
Published: 01 April 2014
Geosphere (2014) 10 (2): 221–232.
...Janet C. Harvey Abstract The Bouse Formation in the lower Colorado River trough holds an important record of the onset of the modern drainage patterns in the southwestern United States. It comprises calcareous and clastic infill deposited during flooding of several basins, including the Bristol...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2010
GSA Bulletin (2010) 122 (9-10): 1625–1636.
... Pliocene Bouse Formation and related units of the lower Colorado River trough (Arizona-California-Nevada), together with parallel oxygen and carbon isotopic analyses of Bouse samples, to constrain the lake-overflow model for integration of the Colorado River. Sr isotopic analyses on the basal 1–5 cm...
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Journal Article
Journal: Geosphere
Published: 01 June 2015
Geosphere (2015) 11 (3): 660–682.
...–0.735; Crossey et al., 2006 ). Speleothem values are 0.713–0.723 ( Hill et al., 2008 ); these are from mammillary coatings on caves interpreted to form near the water table in phreatic groundwater cave systems. Hualapai Limestone 87 Sr/ 86 Sr ranges from 0.7114 to 0.7190, and Bouse carbonates...
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Journal Article
Journal: Geosphere
Published: 01 October 2014
Geosphere (2014) 10 (5): 842–869.
...Kristin McDougall; Adriana Yanet Miranda Martínez Abstract Foraminiferal assemblages in the stratigraphically lower part of the Bouse Formation in the Blythe basin (lower Colorado River corridor, western USA) indicate marine conditions, whereas assemblages in the upper part of the Bouse Formation...
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Journal Article
Journal: Geosphere
Published: 01 December 2014
Geosphere (2014) 10 (6): 1139–1160.
...–370 m asl. There are no Bouse outcrops in the eroded bedrock hills of the Topock paleodivide, and thus no basis for directly estimating the height of the paleodivide to 560 m asl, or 300 m asl as inferred by Turak (2000) and utilized by McDougall and Miranda Martínez (2014) . We group...
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Journal Article
Published: 01 August 1998
Journal of the Geological Society (1998) 155 (4): 697–710.
... Klemenic P.M. Poole S. The geology and geochemistry of upper Proterozoic granitoids from the Red Sea hills, Sudan Journal of the Geological Society, London 1988 145 635 643 Kröner A. Klerkx J. Michot J. Late Precambrian plate tectonics and orogeny: a need to redefine...
Series: GSA Field Guides
Published: 04 September 2019
DOI: 10.1130/2019.0055(03)
EISBN: 9780813756554
... of its upstream lake breached the divide and led the river southward. The Bouse Formation in this and other basins records the pre–river integration water bodies. Younger riverlaid deposits including the Bullhead Alluvium (Pliocene) and the Chemehuevi Formation (Pleistocene) record subsequent evolution...
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.... North of Cottonwood Valley, the Colorado River flows through Black Canyon, which separates this reach of the river from the west-trending reach in the Lake Mead area. The Pyramid hills (informal name) form the boundary between the Cottonwood and Mohave Valleys, and they are composed almost entirely...
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Journal Article
Journal: PALAIOS
Published: 01 March 2016
PALAIOS (2016) 31 (3): 81–91.
...JORDON BRIGHT; ANDREW S. COHEN; DAVID L. DETTMAN; PHILIP A. PEARTHREE; REBECCA J. DORSEY; MINDY B. HOMAN Abstract The southern Bouse Formation (late Miocene–early Pliocene) in Blythe basin, CA-AZ, contains a controversial record of the events that preceded the integration of the developing Colorado...
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Journal Article
Journal: Geosphere
Published: 01 February 2015
Geosphere (2015) 11 (1): 1–30.
... and local deformation. The Bullhead Alluvium is inset into the Hualapai and Bouse Formations along a basal erosional unconformity. Its base defines a longitudinal profile interpreted as the incised end result after the Colorado River integrated through lake basins. Subsequent Bullhead aggradation, at ca...
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Journal Article
Journal: Economic Geology
Published: 01 May 2004
Economic Geology (2004) 99 (3): 561–584.
... of the bare-rock Endeavour segment of the Juan de Fuca Ridge, is host to the base metal-rich (Cu-Zn) Bent Hill massive sulfide deposit. At a water depth of 2,400 m, the ~9 Mt Bent Hill deposit is a steep-sided body ~200 m across and ~100-m-thick. Ocean Drilling Program (ODP) hole 856H penetrates through...
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Journal Article
Journal: Economic Geology
Published: 01 November 2000
Economic Geology (2000) 95 (7): 1473–1488.
...T. Bjerkgård; B. L. Cousens; J. M. Franklin Abstract The Bent Hill and the Ore Drilling Program massive sulfide deposits in Middle Valley, the sediment-filled rift valley at the northern Juan de Fuca Ridge, are among the largest and richest sulfide deposits on the modern sea floor. Drilling during...
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Journal Article
Journal: Economic Geology
Published: 01 August 2014
Economic Geology (2014) 109 (5): 1171–1177.
... of the existing lead isotope data ( Pettke et al., 2010 ), this model may not be incompatible with the previously proposed lower crustal source of metals in Laramide porphyry copper deposits ( Bouse et al., 1999 ; Titley, 2001 ). An important role for subcontinental mantle lithosphere and basal crust...
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Book Chapter

Series: Special Publications of the Society of Economic Geologists, Special Publications of the Society of Economic Geologists
Published: 01 January 2012
DOI: 10.5382/SP.16.01
EISBN: 9781629490410
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Journal Article
Journal: Economic Geology
Published: 01 March 2000
Economic Geology (2000) 95 (2): 361–389.
... and turbiditic sediments from hole 856H, drilled near the summit of the Bent Hill massive sulfide deposit, are similiar to those of sediments in hole 1035H, which was drilled 350 m south of hole 856H near the southernmost peak of the Ocean Drilling Program mound. At both holes, the clay fraction...
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