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Atushi Formation

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Image
Conglomerate clast counting data from the Pliocene <b>Atushi</b> <b>Formation</b> in the ...
Published: 23 May 2019
Figure 7. Conglomerate clast counting data from the Pliocene Atushi Formation in the Wuheshalu section, showing numbers and percentages of different sizes, roundness, and lithologic grades.
Journal Article
Journal: GSA Bulletin
Published: 01 July 2006
GSA Bulletin (2006) 118 (7-8): 1006-1021.
... are also gently dipping and do not show evidence of deformation across the anticlinal core. T3a is gently folded, but the axis of the terrace fold is north of the axial trace of the anticline; T3 dips 3.3° to the south, on Atushi Formation strata dipping ∼0° to the north. No faults were observed...
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Journal Article
Journal: Lithosphere
Published: 23 May 2019
Lithosphere (2019) 11 (4): 507-523.
...Figure 7. Conglomerate clast counting data from the Pliocene Atushi Formation in the Wuheshalu section, showing numbers and percentages of different sizes, roundness, and lithologic grades. ...
FIGURES | View All (8)
Image
Figure 6. Photograph of terraces on the southern limb of the <b>Atushi</b>-Talangh...
Published: 01 July 2006
Figure 6. Photograph of terraces on the southern limb of the Atushi-Talanghe anticline. The cliff in the background is created by the capping conglomeratic Xiyu Formation, which interfingers below with the sandstone and mudstone Atushi Formation. Terrace T3b is broader and more continuous than
Image
Figure 3. CORONA image and simplified geologic map of Kashi-<b>Atushi</b> fold sys...
Published: 01 July 2006
Figure 3. CORONA image and simplified geologic map of Kashi-Atushi fold system. North-directed shortening results in exposed late Cenozoic strata above the Quaternary alluvium. With the exception of the Xiyu Formation, the late Cenozoic sedimentary sequence exposed by the anticlines is easily
Image
Figure 8. Map and profiles of Boguzihe fluvial terraces on the <b>Atushi</b>-Talan...
Published: 01 July 2006
Figure 8. Map and profiles of Boguzihe fluvial terraces on the Atushi-Talanghe anticline. (A) Geologic cross section of the Talanghe anticline (from Scharer et al., 2004 ). Above the modern topography, the structure lines are dotted and the Xiyu Formation is lighter gray. (B) Aerial photograph
Image
(A) Depositional ages of the Xiyu <b>Formation</b> in the western Tarim Basin, inc...
Published: 22 October 2018
Figure 12. (A) Depositional ages of the Xiyu Formation in the western Tarim Basin, including previous studies; magstrat—magnetostratigraphic, TCN—terrestrial cosmogenic nuclides. (B) Initiation ages of different structures within the western Tarim Basin, illustrating basinward propagation
Image
Representative outcrop photographs from the Wuheshalu section. (A) The Pami...
Published: 23 May 2019
of well-developed sandstone sheets indicating transition from the Anjuan Formation to the overlying Pakabulake Formation. (D) Shift from the middle Pakabulake Formation to the upper Pakabulake Formation, with increase of sandstone/mudstone ratio. (E) Conglomerate of the Atushi Formation overlying mudstone
Image
Figure 10. Photographs of terraces on the Mingyaole anticline. (A) A flight...
Published: 01 July 2006
Atushi Formation strata are exposed in the modern riverbed. View is to the north-northwest, located on Figure 9 , and scale is provided by trees partially obscuring scarp. (B) Photograph of terrace T7j, which tilts −5.2° to the north (the tilt relative to the modern stream is −6.2). The Atushi Formation
Image
(A) Simplified geologic map of the southern end of the Kelatuo anticline. (...
Published: 22 October 2018
ratio of the west Atushi (WATSH) sample. Abbreviation: magstrat—magnetostratigraphic age. (D) Photo of the Neogene Atushi Formation and Pliocene–Pleistocene Xiyu Formation. (E) Photo interpretation on D, showing growth strata on the southern flank of the Kelatuo anticline. (F) Magnetostratigraphic
Journal Article
Journal: Geology
Published: 11 September 2018
Geology (2018) 46 (10): 919-922.
...% of land area, and are typically unvegetated and arid desert environments ( Wilson, 1973 ). The Tarim Basin formed between the Tibetan Plateau, Pamir, and Tian Shan orogens, and contains a 3–8-km-thick Cenozoic stratigraphy. Since the early Miocene, the fluvial and lacustrine Wuqia Group, Atushi Formation...
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Journal Article
Journal: Lithosphere
Published: 01 August 2013
Lithosphere (2013) 5 (4): 382-392.
... ) to represent pre-Tertiary to Early Tertiary strata. The Miocene Wuqia Group lies between reflections E and F ( Fig. 3 ), and the Pliocene Atushi Formation ( Fig. 4 ) conformably overlies the Wuqia Group and consists of up to 4000 m of interbedded tan sandstone, siltstone, mudstone, gypsum, and rare pebble...
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Simplified late Cenozoic evolutionary model of the Pamir–South Tian Shan (S...
Published: 23 May 2019
belt also provided a minor amount of detritus to the Wuheshalu area, leading to a mixed provenance and an E-directed paleocurrent direction. (C) During deposition of the upper Atushi Formation, northward thrusting of PFT and Wuheshalu fault (WF) resulted in northward propagation of the North Pamir
Journal Article
Journal: Lithosphere
Published: 22 October 2018
Lithosphere (2018) 10 (6): 806-828.
...Figure 12. (A) Depositional ages of the Xiyu Formation in the western Tarim Basin, including previous studies; magstrat—magnetostratigraphic, TCN—terrestrial cosmogenic nuclides. (B) Initiation ages of different structures within the western Tarim Basin, illustrating basinward propagation...
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Series: SEPM Concepts in Sedimentology and Paleontology
Published: 01 January 2013
DOI: 10.2110/sepmcsp.11.126
EISBN: 9781565762893
... from Wushi, Xinjiang (E4: 41.2°N, 79.2°E), the Wutankule Formation from Atushi, Xinjiang (E5: 39.7°N, 76.1°E). Alsharhan and Nairn (1997, p. 165) cited the Early Permian Dalan Formation. Utha-aroon and Surinkum (1995) cited the Nam Mahoran Formation at Loei (E6: 17.5°N, 101.75°E). Mørk (oral...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2015
GSA Bulletin (2015) 127 (9-10): 1155-1173.
... ( Fig. 3 ). Deposition started during the Late Jurassic to Early Cretaceous with an ∼4-km-thick sequence of conglomerates of the Buenavista Formation, which change laterally to beds of shale and salt, followed by the shale and mudstone-dominated Macanal, Caqueza, and Fómeque Formations ( Fig. 3A ; Mora...
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Journal Article
Published: 06 May 2014
Bulletin of the Seismological Society of America (2014) 104 (3): 1070-1087.
... and formation data for well 11104006. Data taken from Ogle and Hacker (1969) ; fault dip shallowed slightly to match our interpretation. The surface dip measurement from Dibblee and Ehrenspeck (1988) is shown to the left of the well. Ogle and Hacker (1969) observe ∼245  m of repeated section in this well...
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Journal Article
Published: 05 March 2019
Bulletin of the Seismological Society of America (2019) 109 (2): 688-715.
... foreland, the Kazakh platform, and the Tarim basin are of the mid to lower crustal nature (up to 40 km hypocentral depth). This may suggest the presence of remnants of a subducting plate or underplating involved in the formation of the Tien Shan ( Alinaghi and Krüger, 2014 ). For each fault‐rupture...
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Series: Reviews in Economic Geology
Published: 01 January 2016
DOI: 10.5382/Rev.18.06
EISBN: 9781629490922
..., with results indicating ore formation at 28.5 Ma (Y-L. Xie, unpub. data, 2014) at the Lizhuang deposit and 29.9 Ma at the Maoniuping deposit ( Hu et al., 2012 ), respectively. These dates overlap those of the widespread postcollisional magmatism throughout the Qinghai-Tibet plateau area ( Hou et al., 2006...
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Journal Article
Published: 20 November 2017
Geological Magazine (2017) 156 (3): 409-429.
... at 274–280 Ma, and were likely formed by crystal cumulation and fractionation of alkali basalts (Zhang et al. 2008 a ; Wei & Xu, 2011 ; Zou et al. 2015 ). Several granitic intrusions crop out in the Halajun area near the Piqiang complex ( Fig. 1b ), ~120 km NE of Atushi City. They intrude...
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