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Dead Indian Monocline

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Journal Article
Published: 01 December 2019
Rocky Mountain Geology (2019) 54 (2): 47–95.
... the eastern base of the topographic feature called Bald Ridge, also known structurally as Dead Indian monocline. Since the Middle Eocene, the study area has been along the northwestern margin of the Bighorn Basin. Prior to that time, the study area existed near the west–east center of the basin. Bald Ridge...
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Image
Comparative topography between the mountainous Bald Ridge (= <b>Dead</b> <b>Indian</b> mo...
Published: 01 December 2019
Figure 5. Comparative topography between the mountainous Bald Ridge (= Dead Indian monocline) and roughly the northern two-thirds of the study area (within the arrow-bounded, white rectangle) at the interface with today’s Bighorn Basin. View is to the west.
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1957
AAPG Bulletin (1957) 41 (4): 591–626.
... of the Bighorn dolomite. Near Dead Indian Hill the advancing southeastern edge of this bedding thrust sheet passed upward into a shear thrust and thence southeastward onto and across the land surface as an erosion thrust. The South Fork thrust sheet, which underlies and is slightly older than the Heart Mountain...
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Journal Article
Journal: GSA Bulletin
Published: 06 July 2017
GSA Bulletin (2017) 129 (11-12): 1636–1659.
... formed by fast-flowing water are totally absent. Bubble trails and ceiling channels are occasionally observed. The largest group of caves is found in the Judean Desert, west of the Dead Sea basin ( Fig. 8 ). Most of these, including the largest caves, are found along NNE-trending monoclines...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1927
AAPG Bulletin (1927) 11 (7): 705–719.
... is strictly a monoclinal accumulation close to the axis of a syncline. Production comes from the thickened lensed portion of the lower part of the Berea sand found at depths from 2,700 to 3,200 feet. The lens extends parallel to the synclinal axis, over an area 12 miles long by 1 2 mile wide...
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Image
View to the west. Outcrop indicated as Cloverly Formation is near the west-...
Published: 01 December 2019
(1,170 m) above the photographer. Only the eastern base of Bald Ridge is within boundaries of the present study area, but its basic east–west monoclinal structure (as the Dead Indian monocline) is clearly represented in cross section B–B’ from Pierce (1965b) . The importance of Bald Ridge to the present
Journal Article
Published: 01 January 2003
Rocky Mountain Geology (2003) 38 (2): 237–245.
... structures of the Bighorn–Beartooth area, including the Canyon Mouth fold (which intersects the Dead Indian monocline at the Clarks Fork of the Yellowstone River), predate N- to N10°E-trending structures such as the eastern Beartooth fault and Dead Indian monocline. Uplift of the Beartooth Mountains occurred...
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Image
Simplified geologic map of area of South Fork and Heart Mountain detachment...
Published: 01 January 2009
of section shown in those figures. Abbreviations: AP , Abiathar Peak; C , Crandall intrusive center; CC , Cathedral Cliffs; DI , Dead Indian Hill; FC , Fox Creek; HM , Hurricane Mesa; K , northwest-striking Castle fault within South Fork fault allochthon; NW , New World intrusive/volcanic center; P
Journal Article
Journal: GSA Bulletin
Published: 01 May 2005
GSA Bulletin (2005) 117 (5-6): 724–735.
... from the northeast corner of present-day Yellowstone National Park ESE to Dead Indian monocline. It was >20 km wide, bounded to the north by the Beartooth Mountains and to the south by the Absaroka Basin. During the waning stage of the Laramide Orogeny, strata of the plateau were cut by a canyon...
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Journal Article
Published: 01 January 2009
Rocky Mountain Geology (2009) 44 (2): 147–164.
... of section shown in those figures. Abbreviations: AP , Abiathar Peak; C , Crandall intrusive center; CC , Cathedral Cliffs; DI , Dead Indian Hill; FC , Fox Creek; HM , Hurricane Mesa; K , northwest-striking Castle fault within South Fork fault allochthon; NW , New World intrusive/volcanic center; P...
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Journal Article
Published: 01 January 2005
Rocky Mountain Geology (2005) 40 (2): 193–209.
... cover, the late Laramide hinge zone of the north–south-trending Dead Indian monocline somehow interacts with older N60°W trends of the main Beartooth uplift to create a complex interplay of many types, orientations, and scales of fractures. Happy sleuthing! Inclusion of this article in a volume...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 2000
AAPG Bulletin (2000) 84 (3): 360–375.
... at the southeast corner of the uplift by early north-northeast-south-southwest-directed conjugate shears and minor thrusts that are then truncated by east-west-directed compressional features, such as the Dead Indian monocline and Line Creek-Oregon basin thrust ( Figure 13 ) ( Wise, 1983 ). The unique...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1937
AAPG Bulletin (1937) 21 (7): 833–898.
.... Fig. 4. —Map of the Guadalupe Mountains proper, Brokeoff Mountains, Crow Flat. Fig. 12. —A view northeastward from near the Pinnacle along the Huapache monoclinal fold showing exposures of Dog Canyon limestone in Trimble Canyon. This monocline rises more than 1,000 feet above Sotol Basin...
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Journal Article
Published: 01 July 2002
Seismological Research Letters (2002) 73 (4): 470–479.
... them with independently derived geological constraints. Among the historical earthquakes of the region, one that has been widely quoted is the event of 1668 ( Burnes, 1835 ; Bilham, 1998 ); it is also listed in the catalog of Indian earthquakes ( Oldham, 1883 ). Our search for historical...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2010
GSA Bulletin (2010) 122 (3-4): 595–608.
... enough to have captured the ancestral Colorado River east of the Shivwitz Plateau. As such, they propose that water from the ancestral Colorado River most likely ponded into a lake that grew deep enough to drain catastrophically over the southeastern limb of the Kaibab Monocline to begin carving...
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Journal Article
Published: 02 May 2013
Geological Magazine (2013) 150 (6): 986–1001.
... 13 11 2012 24 01 2013 Copyright © Cambridge University Press 2013 2013 Cambridge University Press In the NW corner of the Deba block, the Aitzeta monoclinal syncline ( Figs 1 b, 4 ) appears adjacent and parallel to the Mutriku fault (Agirrezabala et al . 2002...
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Series: GSA Field Guides
Published: 04 September 2019
DOI: 10.1130/2019.0055(03)
EISBN: 9780813756554
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Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2014
DOI: 10.1306/13431859M1063609
EISBN: 9781629812663
... domain, which became connected to the western Indian Ocean through the Gulf of Aden ( Stampfli et al., 2001 ). Figure 3. Triassic isopach map of the Levant region showing the major oil and gas fields, the extent of the Kurrachine evaporites, and the locations of the wells producing from Triassic...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 2002
AAPG Bulletin (2002) 86 (12): 2023–2045.
... the Assam valley on the southeast and extends southwestward across northern and western Myanmar (Burma). The thrust belt developed as a result of differential movement between the Burma microplate and the Indian plate. Prior to collision of the Burma microplate, what is now the western part of the thrust...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1948
AAPG Bulletin (1948) 32 (7): 1227–1264.
... in contemporaneous deposition away from the dome. In the Gulf Coast the regional geology is very simple (monoclinal dip toward the coast), extensive drilling has been done around domes, and detailed subsurface studies made by use of paleontology and electric logs. This work has clearly established the three...
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