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Lishan Mountains

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Journal Article
Journal: Geology
Published: 01 September 2012
Geology (2012) 40 (9): 831–834.
... to the onset of arc-continent collision ca. 6.7 Ma has been identified in rift basins of the southern Chinese margin near Taiwan, further suggesting that collision may be preceded by bending-related extension of the continental shelf. The Lishan fault, a major structural and morphologic boundary in the Taiwan...
FIGURES
Journal Article
Journal: Geology
Published: 01 August 2009
Geology (2009) 37 (8): 711–714.
... direction determined by these methods. Figure 2 A: Joint transverse electric, transverse magnetic, and tipper inversion model. FBC—Foreland Basin conductor; LFC—Lishan fault conductor; LVC—Longitudinal Valley conductor; CP—Coastal Plain; WF—Western Foothills; HSR—Hseuhshan Range; LF—Lishan fault...
FIGURES
Journal Article
Published: 15 February 2024
Seismological Research Letters (2024)
... to the northwest within the WHG. The Lishan horst on the footwall of the fault experienced a significant sinking from the Eocene relative to the Qinling Mountains. This subsidence slowed down notably in the Pliocene, but then the uplift accelerated relative to the Xi’an depression ( SSBO, 1988 ). Over time...
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Image
Simplified geological map of the Taiwan <span class="search-highlight">mountain</span> belt (modified after  Chen...
Published: 12 September 2013
Fig. 1. Simplified geological map of the Taiwan mountain belt (modified after Chen et al . 2000 ). The locations of the study area in Figure 2 and of the crustal cross-section in Figure 12 are shown. Contours offshore indicate the thickness (in km) of the Palaeocene to Miocene sediments
Journal Article
Journal: Geology
Published: 01 February 2014
Geology (2014) 42 (2): 147–150.
... it was followed by more than 680 aftershocks that ranged to 5 M L . Most events occurred below the ∼10-km-deep detachment fault predicted for this part of the mountain belt, coinciding with other precisely located hypocenters that indicate that much of the crust in this area is seismically active. We combine...
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Image
Figure 1. (A) Map of Taiwan and surrounding region, showing the tandem sutu...
Published: 01 November 2006
Range (CoR), the docked part of the Luzon volcanic arc, and the continental sliver of the Central Range (CeR), the mountainous backbone of the island. Current velocity vectors of the Philippine Sea plate relative to South China, at 124°E and 20°, 21°, and 22°N, are calculated using the Recent plate
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 February 2013
Lithosphere (2013) 5 (1): 49–66.
... , v. 22 , no. 3 , 1025 , doi:10.1029/2002TC001436 . Lee J.C. Angelier J. Chu H.T. , 1997 , Polyphase history and kinematics of a complex major fault zone in the northern Taiwan mountain belt: The Lishan fault : Tectonophysics , v. 274 , p. 97 – 115 , doi:10.1016/S0040-1951...
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Journal Article
Published: 13 January 2021
Seismological Research Letters (2021) 92 (3): 1992–2003.
..., and the resultant deformation does not resemble a typical plate boundary collision. In addition, the existence of the Lishan fault forms a boundary that resists the northwestward movement of the block ( Kuo‐Chen et al. , 2015 ). The region then slides clockwise along the boundary. There are fewer earthquakes from...
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Journal Article
Published: 12 September 2013
Journal of the Geological Society (2014) 171 (1): 117–130.
...Fig. 1. Simplified geological map of the Taiwan mountain belt (modified after Chen et al . 2000 ). The locations of the study area in Figure 2 and of the crustal cross-section in Figure 12 are shown. Contours offshore indicate the thickness (in km) of the Palaeocene to Miocene sediments...
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Series: Geological Society, London, Special Publications
Published: 01 January 2011
DOI: 10.1144/SP359.14
EISBN: 9781862396074
... source Meteoric d Meteoric e Major vein systems (fluid-flow zones) Inboard Focused vein swarms Fracture-controlled; dispersed f , g Outboard Lishan Fault; locally focused zones in mountains Outboard faults h − j Fluid source Mainly shallow meteoric; some deep-sourced brines...
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Journal Article
Published: 01 June 2006
Journal of Environmental and Engineering Geophysics (2006) 11 (2): 73–81.
... in the northern Lishan Mountains, 35 km east of Xi'an ( Fig. 1 ). The geographic coordinates are longitude 109°11′–109°21′ East and latitude 34°21′–34°27′ North. Materials from the ground surface to the depth of around 400 m are loess, clay loess, sandy soil, and gravel beds. A regional aeromagnetic survey...
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Journal Article
Published: 04 March 2020
Seismological Research Letters (2020) 91 (3): 1469–1481.
...Ming‐Che Hsieh; Yen‐Yu Lin; Kuo‐Fong Ma; Li Zhao; Yi‐Wun Liao Abstract Seismically active central Taiwan is considered part of an orogenic wedge with low‐angle east‐dipping active faults above a detachment surface and an active mountain‐building process later. In 2013, two moderate reverse‐faulting...
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Series: GSA Special Papers
Published: 01 January 2008
DOI: 10.1130/2008.2436(12)
... of the southern basin margin to the east and southeast. We propose that the Ilan Basin is being formed as a result of extension of northern Taiwan, largely controlled by a major southeast-dipping fault, modeled at ∼30° dip, and mapped as a continuation of the Lishan Fault, a major thrust structure in the Central...
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Journal Article
Published: 11 July 2019
Geological Magazine (2021) 158 (1): 84–103.
... and Chu H-T ( 1997 ) Polyphase history and kinematics of a complex major fault zone in the northern Taiwan mountain belt: the Lishan Fault . Tectonophysics 274 , 97 – 115 . Lester R , McIntosh K , Van Avendonk HJA , Lavier L , Liu C-S and Wang TK ( 2013...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2010
GSA Bulletin (2010) 122 (7-8): 1192–1208.
... or to widen its banks) and is undammed, making it a suitable river to investigate channel dynamics in response to active deformation in this region of Taiwan. The river headwaters are located in the Eocene-Oligocene metasedimentary rocks of the Lishan valley, formed by the east-verging Lishan thrust ( Fig. 1...
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Journal Article
Journal: Geology
Published: 01 February 2000
Geology (2000) 28 (2): 155–158.
... Proceedings , v. v. 31 pp. 209 ߝ 230 . Lee , J.C. , Angelier , J. , and Chu , H.T. , 1997 , Polyphase history and kinematics of a complex major fault zone in the northern Taiwan mountain belt: The Lishan fault : Tectonophysics , v. v. 274 pp. 97 ߝ 115 . Lewis , S.D...
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Journal Article
Published: 09 August 2022
Geological Magazine (2022) 159 (10): 1663–1680.
... the Panjiaduan Cu–Pb–Zn deposit (modified from Mamyrin & Tolstihkin, 1984 ). The He–Ar isotopic compositions of typical Pb–Zn polymetallic vein-type deposits including the Tighza-Jbel Aouam, Iheya and Lishan deposits are from Yang et al. ( 2021 ), Rossi et al. ( 2017 ) and Yu et al. ( 2021...
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Journal Article
Journal: GSA Bulletin
Published: 16 October 2023
GSA Bulletin (2024) 136 (5-6): 2494–2508.
...) Geological map of the study area in Lishan, Sulu belt (modified after Xu et al., 2016 ). The Shidao Complex is ~300 km 2 in size and has three phases, including gabbro, syenite, and granite. The syenite unit is composed of pyroxene-, amphibole-, and quartz-syenite ( Xu et al., 2016 ). (C) Newly discovered...
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Journal Article
Journal: Geology
Published: 06 June 2023
Geology (2023) 51 (8): 785–790.
...-Tethys and Paleo-Pacific supra–subduction zone setting. Our revision locates SW Borneo with other SE Tethysides blocks in Eurasia where accretionary orogens have influenced rises after 200 Ma. * lishan@ucas.ac.cn 27 11 2022 12 4 2023 22 5 2023 © 2023 Geological Society...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2006
GSA Bulletin (2006) 118 (11-12): 1447–1462.
... Range (CoR), the docked part of the Luzon volcanic arc, and the continental sliver of the Central Range (CeR), the mountainous backbone of the island. Current velocity vectors of the Philippine Sea plate relative to South China, at 124°E and 20°, 21°, and 22°N, are calculated using the Recent plate...
FIGURES | View All (13)