Wildcat Mountain Fan

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Map of <b>Wildcat</b> <b>Mountain</b> <b>fan</b> plotted on basemap for Denver Basin. Net sandst...
Published: 01 January 2003
Figure 5. Map of Wildcat Mountain fan plotted on basemap for Denver Basin. Net sandstone thicknesses within fan were measured in 140 wells (dots). Lobate feature extending from Wildcat Mountain comprises majority of porous and permeable components of Arapahoe aquifer in mapped area. Southern
<b>Wildcat</b> <b>Mountain</b> <b>fan</b> in cross section (line of section shown in  Fig. 5 ). ...
Published: 01 January 2003
Figure 6. Wildcat Mountain fan in cross section (line of section shown in Fig. 5 ). Multistoried and coalesced sandstone bodies characterizing proximal fan environments are transitionally replaced distally to northeast by less amalgamated, more isolated sandstone layers. Water-well performance
Journal Article
Journal: Geology
Published: 01 June 1996
Geology (1996) 24 (6): 559–562.
...David A. Ferrill; John A. Stamatakos; Sidney M. Jones; Bret Rahe; H. Lawrence McKague; Ronald H. Martin; Alan P. Morris Abstract Analyses of alluvial fan sedimentation around Bare Mountain, Nevada, indicate differential slip along the Bare Mountain fault during the Pleistocene and Holocene...
Journal Article
Published: 01 December 2010
Journal of Sedimentary Research (2010) 80 (12): 1085–1108.
... submarine channel-belt in the Magallanes retro-arc foreland basin on Sierra del Toro represent the fill of a 3.5 km wide, 300 m thick channel complex, here termed the “Wildcat,” that displays an asymmetric cross section and facies distribution. Measured sections and mapping demonstrate that facies...
FIGURES | View All (17)
Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2410(22)
... showing plate boundaries and general outcrop areas of the Eel River basin, Wildcat Group (Tw), Klamath Mountains and Coast Ranges provinces and location of the Mendocino triple junction (at Cape Mendocino). SAf—San Andreas fault. He further defined the “Bellspring peneplain” as having formed west...
FIGURES | View All (9)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1956
AAPG Bulletin (1956) 40 (8): 1945–1967.
.... The source of these sediments was the Amarillo mountains, and nearer the mountains are the thicker parts of these wedge- or fan-like lenses of granite wash. This clastic section includes Pennsylvanian rocks of pre-Des Moines, Des Moines, Missouri, and Virgil, and even Lower Permian age. These wedges...
FIGURES | View All (9)
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1944
AAPG Bulletin (1944) 28 (6): 806–833.
.... The 111 West Texas wildcats resulted in 17 new discoveries, representing a success of 15.32 per cent, while in New Mexico 37 wildcats found 6 new pools representing 16.22 per cent exploratory success. Total pipe-line runs in West Texas of 98,070,000 barrels were 17,040,000 barrels more than in 1942, while...
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1978
AAPG Bulletin (1978) 62 (11): 2243–2274.
..., fractured, siliceous shales deposited beyond distal margins of the fan complex. Many underexplored areas remain in the San Joaquin Valley despite many years of field development and wildcat drilling. The Miocene of the Bakersfield arch is representative of the classic arcuate type of turbidite deposits...
FIGURES | View All (23)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1990
AAPG Bulletin (1990) 74 (9): 1371–1385.
... of a lacustrine/swamp system. Concurrently, parts of some valleys were being filled by coarse sediment, some of which was emplaced by debris flows. Several fan deltas, fed by mountain streams, began building to the southwest into the lacustrine/swamp system. As progradation continued, the lacustrine/swamp...
FIGURES | View All (13)
Published: 01 December 2007
DOI: 10.5724/gcs.07.27.0081
EISBN: 978-0-9836096-3-6
... sequences. Each unit is defined by relevant biostratigraphic control, sequences and systems tracts, depositional systems, and sedimentary processes. On the basin floor, early lowstand sandy turbidite sequences are characterized as channelized fan systems or distributary fan systems. Sand-poor intervals...
Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2005
DOI: 10.1144/GSL.MEM.2005.031.01.07
EISBN: 9781862394063
... Trench (Fig. 7.1 ). The continental margin of SE Asia is of Andean type, with active and inactive Quaternary volcanoes rising to over 3000 m above a Pre-Tertiary basement, exposed towards the west coast of the island in the Barisan Mountains. Tertiary sedimentary basins occur both to the SW and the NE...
FIGURES | View All (8)
Journal Article
Journal: Geosphere
Published: 08 December 2017
Geosphere (2018) 14 (1): 74–94.
... in composition from tholeiitic basalt (Spring Mountain) to calc-alkaline basaltic andesite through dacite (Lava Mountain, Crescent Mountain, and Wildcat Hill), and include a lamprophyre intrusion (Pilot Knob). Together, these igneous rocks define the Upper Wind River Basin volcanic field (UWRB). All UWRB rocks...
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Series: SEPM Field Trip Guidebook, SEPM Field Trip Guidebook
Published: 01 January 2009
DOI: 10.2110/sepmfg.10.031
EISBN: 9781565762923
... Figure 6.3. Lithofacies and other features of the Condor channel complex margin. Parts A–E are from the north face of Sierra del Toro; Parts F–I feature exposures of the margin on the south face of the mountain. (A) Despite modification by post-depositional faulting (faults indicated by yellow...
Series: GSA Field Guide, GSA Field Guide
Published: 01 January 2017
DOI: 10.1130/2017.0048(01)
... of ductile detachment levels and correlation to timing of Rocky Mountain thrust systems (SFA—Selkirk Fan; PU—Purcell thrust; PCA—Porcupine Creek Anticlinorium—PCA; SMt—Sulphur Mountain thrust; Ru—Rundle thrust; see Figure 13 for other abbreviations); modified from Simony and Carr (2011) . Figure...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 2013
AAPG Bulletin (2013) 97 (6): 899–921.
... accumulation. Conglomerates were deposited on alluvial fans and braid plains along the mountain front ( Lawton, 1985 ); they probably represent locations of major hinterland-draining rivers that exited the Cordillera at transfer zones between thrust salients ( Lawton et al., 1994 ). The small size of channels...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2005
GSA Bulletin (2005) 117 (5-6): 570–588.
...Jeffrey M. Tropaff; Darren A. Szuch; Matthew Rioux; Robert B. Blodgett Abstract Analysis of the Upper Jurassic Naknek Formation in the Talkeetna Mountains, Alaska, documents synorogenic sedimentation in a forearc basin along the outboard (southern) margin of the allochthonous Peninsular terrane...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1997
AAPG Bulletin (1997) 81 (7): 1133–1160.
... holes near Del Norte, Colorado, led to seismic exploration and petroleum wildcat drilling in the volcanic field ( Gries, 1985 , 1989 ) and to the confirmation of this Rocky Mountain Laramide sedimentary basin. A subsequent 6 yr period of wildcat drilling revealed the presence of several thousand...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1967
AAPG Bulletin (1967) 51 (10): 1979–2032.
...Perry O. Roehl ABSTRACT During Late Ordovician and Silurian times, epeiric carbonate sediments were deposited over a negative metastable lineament of the western Williston basin. These sediments are now the Stony Mountain Formation and Interlake Formation dolomites. The original sedimentary...
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