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Calico Member

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Journal Article
Journal: Geosphere
Published: 01 June 2008
Geosphere (2008) 4 (3): 459–479.
... most of the Calico Mountains, volcaniclastic sediments and dacitic rocks of the Pickhandle Formation accumulated rapidly between ca. 19.4 and 19 Ma. Overlying fine-grained lacustrine beds (here referred to as the Calico Member of the Barstow Formation) are bracketed between ca. 19 and 16.9 Ma...
FIGURES | View All (14)
Image
Figure 7. Selected views of folds in the <b>Calico</b> <b>Member</b>. (A) Folded lacustri...
in > Geosphere
Published: 01 June 2008
Figure 7. Selected views of folds in the Calico Member. (A) Folded lacustrine rocks in the Calico Ghost Town parking lot. The photo is a composite of three shots with distortion. The line drawing is a composite profile view sketch that is approximately true to scale. View is looking west. (B
Image
Figure 10. Contact between the <b>Calico</b> <b>Member</b> and overlying dacite breccia (...
in > Geosphere
Published: 01 June 2008
Figure 10. Contact between the Calico Member and overlying dacite breccia (Tdb). Note that Calico beds become more shallowly dipping closer to the contact. The solid white line marks the Calico Member–dacite breccia contact. Dashed white lines are form lines in the Calico Member. View is looking
Image
The <b>Calico</b> sandstones (here two can be seen) of the Smoky Hollow <b>Member</b> are...
Published: 01 May 2002
Figure 4 The Calico sandstones (here two can be seen) of the Smoky Hollow Member are shown underlying the erosively based A sandstone complex. A sequence boundary lies between these two prominent units, and this can be traced extensively around the Plateau.
Image
—One of several ripple-marked fields in <b>Calico</b> Rock Sandstone <b>Member</b>. Geolo...
Published: 01 April 1974
Fig. 10. —One of several ripple-marked fields in Calico Rock Sandstone Member. Geologic section 20 on White River, Baxter County, Arkansas.
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1974
AAPG Bulletin (1974) 58 (4): 685–707.
...Fig. 10. —One of several ripple-marked fields in Calico Rock Sandstone Member. Geologic section 20 on White River, Baxter County, Arkansas. ...
FIGURES | View All (20)
Image
Figure 9. Simplified map of the southern <b>Calico</b> Mountains illustrating geom...
in > Geosphere
Published: 01 June 2008
Figure 9. Simplified map of the southern Calico Mountains illustrating geometry and map view pattern of folds in the Calico Member. Fold axial traces parallel the overall contact with Yermo dacite rocks (Ty), and in any given structural domain, folds have consistent orientations. (A) Inset
Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP444.1
EISBN: 9781786203748
... unconformably on the Calico Bed of the Smoky Hollow Member. These barforms are overlain by carbonaceous estuarine bay fill with tidal deposits, a bayhead delta and, ultimately, a coastal plain succession. The estuarine succession demonstrates a decreasing tidal influence through time and this is interpreted...
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Journal Article
Published: 01 November 2016
Journal of Sedimentary Research (2016) 86 (11): 1310–1327.
... comprising these depositional units are summarized below. The lowermost depositional unit, DU-0, is 10 to 20 m thick and forms a prominent cliff that overlies the Calico Bed of the Smoky Hollow Member. The unit contains thick and laterally extensive channel belts consisting of coarse-grained sandstones...
FIGURES | View All (13)
Journal Article
Journal: GSA Bulletin
Published: 23 June 2017
GSA Bulletin (2017) 129 (9-10): 1027–1051.
... the northern McDermitt volcanic field, through McDermitt caldera and the Santa Rosa–Calico center, to the northern Nevada Rift. A similar linear trend is observed ∼75 km to the west, where the Hawks Valley–Lone Mountain center and the calderas of the High Rock caldera complex define an ∼N20°E trend radiating...
FIGURES | View All (14)
Journal Article
Journal: GSA Bulletin
Published: 01 January 2000
GSA Bulletin (2000) 112 (1): 34–44.
...-south shortening along the northwest-striking Calico fault, which in this area accommodated about 10 km of right slip and perhaps 1 km of reverse slip. Southwestward-dipping strata in the areally extensive north limb of the syncline resemble tilted strata in nearby highly extended areas and have been...
FIGURES | View All (7)
Journal Article
Journal: Geosphere
Published: 17 July 2017
Geosphere (2017) 13 (4): 1066–1112.
..., but the caldera is younger than two known calderas in northwestern Nevada. Published data show that silicic activity as old as at McDermitt is also found from the Silver City area of southwestern Idaho to the Santa Rosa–Calico volcanic field in Nevada east of McDermitt. As recognized by others, an area of ∼40,000...
FIGURES | View All (19)
Image
—Outcrop of Everton Formation exposing Sneeds Dolomite <b>Member</b> (S), limeston...
Published: 01 April 1974
Fig. 6. —Outcrop of Everton Formation exposing Sneeds Dolomite Member (S), limestone-sandstone member A (A), Calico Rock Sandstone Member (C). Calico Rock, Izard County, Arkansas.
Image
—Stromatolites in medium crystalline dolomite in Sneeds Dolomite <b>Member</b>. On...
Published: 01 April 1974
Fig. 9. —Stromatolites in medium crystalline dolomite in Sneeds Dolomite Member. Onkolites are overlain by laterally linked hemispheroids. Calico Rock, Izard County, Arkansas.
Image
— A.  Sneeds Dolomite <b>Member</b>. Finely crystalline dolomite with stringer of ...
Published: 01 April 1974
with oolitic rims. Ordinary light. C. Sandstone characteristics of Calico Rock and Newton sandstones. Quartz grains have well-defined dust rings and interlocking quartz overgrowths that provide cement. Crossed nicols. D. Member B. Calcarenite with intraclasts of various sizes and shapes, ostracods
Image
Figure 8. (A) Poles to measured bedding attitudes in the Pickhandle Formati...
in > Geosphere
Published: 01 June 2008
Figure 8. (A) Poles to measured bedding attitudes in the Pickhandle Formation. Beds generally dip 15–30°S to SE and are not folded. (B) Poles to bedding attitudes in the folded Calico Member north of the Calico fault. Figure only shows attitudes plotted in Plate 1 and does not include bedding
Journal Article
Published: 01 October 2015
Journal of Sedimentary Research (2015) 85 (10): 1166–1196.
... proximal shoreface and nonmarine sedimentation. The Smoky Hollow Member comprises carbonaceous floodplain mudstones and thin coals interbedded with isolated fluvial channels ( Peterson 1969b ). Amalgamated, coarse-grained fluvial channels of the Calico Bed commonly mark the top of the Smoky Hollow Member...
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Series: GSA Memoirs
Published: 01 January 2007
DOI: 10.1130/2007.1199(03)
...) the Calico Hills Formation, Yucca Mountain Tuff, and crystal-poor members of the Tiva Canyon and Topopah Spring Tuffs are predominantly high-silica rhyolites; (2) tuffs in the Crater Flat Group exhibit a compositional range that is between high- and low-silica rhyolites; (3) the Lithic Ridge and Pah Canyon...
FIGURES | View All (19)
Journal Article
Published: 01 March 2016
Journal of Sedimentary Research (2016) 86 (3): 125–147.
..., a localized channel belt (∼ 1150 m wide and 5 m thick) at the base of the John Henry Member unconformably overlies the Smoky Hollow Member ( Fig. 4 ). Throughout most of this study area the basal John Henry Member sandstone completely removes the underlying Calico bed (∼ 4 m thick where preserved; Fig. 6E...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1965
AAPG Bulletin (1965) 49 (2): 172–185.
... alternation with dark gray shale produces striped exposures that closely resemble the Calico Bluff Formation of Late Mississippian age at its spectacular type locality 5 miles west of McCann Hill. The limestone and shale member of the McCann Hill Chert is about 250 feet thick near Benchmark 4085 and along...
FIGURES | View All (5)