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Jianshan China

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Journal Article
Published: 01 November 2022
The Journal of Geology (2022) 130 (6): 499–518.
... not been reached. The Jianshan BIF is in the southern section of the Yuanjiacun-Jianshan iron metallogenic belt in the central North China Craton (NCC). In comparison, previous studies on BIFs in this region mostly focused on the Yuanjiacun BIF in the southern section, based on which they explicitly...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 29 January 2022
Lithosphere (2021) 2021 (Special 4): 6426550.
... provide theoretical guidance and technical support for the stability analysis of open-pit high slopes under blasting vibration. The Dianchi Lake area of Yunnan Province is one of the main distribution areas of phosphate deposits in China. These include the Jianshan Phosphate Mine and Kunyang...
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First thumbnail for: Study on Three-Dimensional Dynamic Stability of Op...
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Journal Article
Journal: AAPG Bulletin
Published: 15 May 2020
AAPG Bulletin (2020) 104 (5): 1091–1113.
... Corridor, and Subei basin, northwest China : American Journal of Science , v.  311 , no.  2 , p.  116 – 152 , doi: 10.2475/02.2011.02 . Figure 8 presents a resulting kinematic forward model that represents the main geometric components of the Jianshan structure. The initial wedge includes a fore...
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First thumbnail for: Development and growth of basement-involved struct...
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Journal Article
Journal: GSA Bulletin
Published: 05 August 2020
GSA Bulletin (2021) 133 (3-4): 802–818.
... and zircon U-Pb-Hf isotopic study of (meta-)sedimentary and volcanic rocks from the Bainaimiao arc terrane and northern margin of the North China craton in the Damao region. The lower and middle successions of the Bayan Obo Group from the northern North China craton, including the Dulahala, Jianshan...
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First thumbnail for: Tectonic origin of the Bainaimiao arc terrane in t...
Second thumbnail for: Tectonic origin of the Bainaimiao arc terrane in t...
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Journal Article
Journal: Geology
Published: 30 October 2024
Geology (2025) 53 (2): 119–124.
... to a lack of geophysical constraints. The world’s largest REE deposit, Bayan Obo of the North China craton, offers a template for tracing such a system using 2-D electrical resistivity imaging. We first restore modifications triggered by two newly discovered Mesozoic thrust faults. The thrust fault along...
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First thumbnail for: Translithospheric carbonatite magmatic system of t...
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Journal Article
Journal: GSA Bulletin
Published: 18 March 2021
GSA Bulletin (2021) 133 (11-12): 2612–2624.
... suture; JSS—Jinsha suture; QT—Qiangtang terrane; SG—Songpan–Ganzi Terrane; Qdm—Qaidam Basin; DBZ—Duobuza; JC—Jiacha; BSG—Baishagang; LGL—Lagala; YLS—Yulinshan; JS—Jianshan; YBCK—Yibuchaka; EJMM—Ejumaima; ZGYCC—Zougouyouchacuo; NDC—Nadingcuo. Ages of the Early Cretaceous–Paleocene mafic rocks are from...
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First thumbnail for: Late Eocene post-collisional magmatic rocks from t...
Second thumbnail for: Late Eocene post-collisional magmatic rocks from t...
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Journal Article
Journal: GSA Bulletin
Published: 09 March 2020
GSA Bulletin (2020) 132 (9-10): 2135–2153.
...Chaohui Liu; Guochun Zhao; Fulai Liu; Jianrong Shi; Lei Ji Abstract Statherian through Tonian strata of the Langshan–Zha’ertai–Bayan Obo–Huade rift zone (LZBH) at the northern margin of the North China Craton provide an excellent record of changes in sediment provenance related...
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First thumbnail for: Detrital zircon records of late Paleoproterozoic t...
Second thumbnail for: Detrital zircon records of late Paleoproterozoic t...
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Journal Article
Journal: Geophysics
Published: 04 October 2013
Geophysics (2013) 78 (6): D429–D444.
... Shizishan line 26–28 stope 8 50,390 120,900 228 75 Jianshan line 30–34 stope 8 30,500 100,000 269 90 This work was supported by grants from the Natural Science Foundation of Hubei Province (no. 2011CDA123) and the Geological Survey Project of China (no. 12120113101800). The authors...
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First thumbnail for: Magnetization vector imaging for borehole magnetic...
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Journal Article
Published: 01 November 2022
The Journal of Geology (2022) 130 (6): i–ii.
..., mokhles azer, and abdel-aal abdel-karim 499 Geology and Geochemistry of the Jianshan Banded Iron Formation in Shanxi Province, China: Constraints on the Genesis yekai men, zijun mi, ende wang, liangde han, yanjie wang, sanshi jia, jianming xia, and kun song ...
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Sketch map of eastern China, showing the distribution of Late Mesozoic adakites, modified after Zhang et al. (2001). Three belts of Mesozoic adakites are distributed in eastern China: the Jurassic adakite belt along the northern margin of the North China Craton (NCC) and Early Cretaceous adakite belts along the Shandong Peninsula and the Xu-Huai region (∼130 Ma) and the Lower Yangtze River Belt (LYRB; ∼140 Ma). Also plotted are three Cretaceous intrusions (Liguo, Banjing, and Jiagou) in the Xu-Huai region, northern Jiangsu and Anhui Provinces, where eclogitic xenoliths were sampled and analyzed in this study. A series of thrust faults were developed there, forming arc-shaped structures (Xu et al. 1987). Squares represent plutonic (intrusive) rocks, while the circles represent volcanic (extrusive) rocks, both of which are shown in different colors in the three adakite belts. JSF = Jianshan-Shaoxing Fault; TLF = Tan-Lu Fault; XGF = Xiangfan-Guangji Fault.
Published: 01 March 2013
Figure 1. Sketch map of eastern China, showing the distribution of Late Mesozoic adakites, modified after Zhang et al. ( 2001 ). Three belts of Mesozoic adakites are distributed in eastern China: the Jurassic adakite belt along the northern margin of the North China Craton (NCC) and Early
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Comparison of temporal variations in δ13Ccarb from the different sections during the transition from the Ediacaran and Cambrian of (1) the Yangtze Platform, China: Shatan (Guo et al.2007), Songtao (Guo et al.2007), Yanwutan-Lijiatuo (Guo et al.2007), Longbizui (Guo et al.2013), Yuanjia (Guo et al.2013), Xiaotan (Li et al.2013), Wuliu–Zengjiayan (Guo et al. 2010), Jianshan (Guo et al.2010a , b) and Wangcun sections (Zhu et al.2004); (2) the Tarim Basin, China: Penglaiba (this study), Wushi phosphrite (this study) and Dongergou sections (this study); (3) USA: Rocky Mountain section (Montañez et al.2000); (4) Russia: Molodo section (Shabanov et al.2008); and (5) Canada: Sekwi Formation (Dilliard et al.2007).
Published: 10 April 2017
al. 2013 ), Yuanjia (Guo et al. 2013 ), Xiaotan (Li et al. 2013 ), Wuliu–Zengjiayan (Guo et al. 2010), Jianshan (Guo et al. 2010 a , b ) and Wangcun sections (Zhu et al. 2004 ); (2) the Tarim Basin, China: Penglaiba (this study), Wushi phosphrite (this study) and Dongergou sections
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 May 2017
Lithosphere (2017) 9 (4): 583–594.
...′ ( Fig. 4F ) shows the geometry of the southeastern segment of the Dafengshan anticline and the middle segment of the Jianshan anticline. In this section, the positive flower geometry of these two anticlines is clear; one is asymmetric and tilts toward the southwest and the other is symmetric. The growth...
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First thumbnail for: Basement controls on deformation during oblique co...
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Journal Article
Published: 01 May 2011
Journal of Paleontology (2011) 85 (3): 567–586.
..., China. Figured material in this paper is identified by the prefix “JS” which stands for Jianshan section. Forty-three specimens show evidence of soft-part preservation. Camera lucida drawings were made for these specimens. All specimens examined in this study are preserved as partly flattened...
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First thumbnail for: A New Arthropod Jugatacaris agilis n. gen. n. sp. ...
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Journal Article
Published: 01 July 2016
Journal of Paleontology (2016) 90 (4): 663–671.
... unguispinus Cong et al., 2014 from the Chengjiang biota, eastern Yunnan Province, China, by original designation. Radiodontan with a pronounced, four-segmented neck; the head bears an oval to subcircular dorsal plate; mouth sub-circular to quadratic in outline, characterized by concentric wrinkled...
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First thumbnail for: Morphology of the radiodontan Lyrarapax from the e...
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Journal Article
Published: 01 November 2007
Journal of Paleontology (2007) 81 (6): 1412–1422.
...., Ma'anshan, Xiaolantian and Jianshan. Detailed information on these localities can be found in Zhang et al. (2001) . Sunellid arthropods, members of the family Sunellidae Huo, 1965 , appear to be relatively important elements of the Cambrian fauna in China. More than 100 individuals...
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First thumbnail for: SOFT ANATOMY OF SUNELLID ARTHROPODS FROM THE CHENG...
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Journal Article
Published: 13 December 2022
Journal of the Geological Society (2023) 180 (1): jgs2021-164.
... . maotianshanensis . Occurrence . Maotianshan Shale Member, Yu'anshan Formation, Jianshan, Haikou, Yunnan, China, Cambrian Series 2, Stage 3. Innovatiocaris ? multispiniformis sp. nov. Figure 14 LSID . urn:lsid:zoobank.org:act:27E62189-0FDE-4599-B64D-49B054668A7D Derivation of name...
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First thumbnail for: Innovatiocaris , a complete radiodont from the ear...
Second thumbnail for: Innovatiocaris , a complete radiodont from the ear...
Third thumbnail for: Innovatiocaris , a complete radiodont from the ear...
Journal Article
Journal: AAPG Bulletin
Published: 12 May 2021
AAPG Bulletin (2021) 105 (5): 883–917.
... is surrounded by the Tarim plate to the northwest, the North China plate to the northeast, and the Qiangtang massif to the south ( Li et al., 2014 ). This basin covers an area of 121,000 km 2 and is filled with a set of continuous Cenozoic lacustrine sedimentary units ( Xia et al., 2001 ; Molnar, 2005 ; Fang...
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First thumbnail for: Resource potential of the Jurassic gas system, nor...
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(A) Geographic location of the present-day Qiantang River (QR) estuary on a Google Earth satellite map, to the west of the East China Sea and immediately south of the Changjiang River delta. Note that the turbid water in the modern QR estuary does not end sharply, as suggested by the image; this is an artifact of Google map-preparation techniques. (B) Locations of the SE2 core, boreholes, shallow biogenic gas fields, and transects in the modern QR estuary region (modified from Lin et al., 2005). (C) Spatial variation in the mean tidal range (units for the isotidal lines are in m) and bottom-sediment types within the present-day QR estuary (modified from Fan et al., 2012). (D) Close view of the Jianshan area on a Google Earth satellite map (see location in C). The sediments are composed of subtidal silty sands and intertidal mudflats. The mudflats have a maximum width of 2.5 km and a total area of &gt;2.5 km2. (E) Close view of the intertidal flat in the Andong wetland on a Google Earth satellite map (see location in C). The intertidal flat has a maximum width of 6.5 km and a total area of 128.7 km2. CD—Changjiang River delta; QR—Qiantang River; HZB—Hangzhou Bay; BCZ—bedload convergence zone; AW—Andong wetland; QRIV—Qiantang River incised valley; THIV—Taihu incised valley; IF—intertidal flat; SZ—subtidal zone. Italics are used to mark the place names mentioned in this paper.
Published: 01 March 2014
Figure 1. (A) Geographic location of the present-day Qiantang River (QR) estuary on a Google Earth satellite map, to the west of the East China Sea and immediately south of the Changjiang River delta. Note that the turbid water in the modern QR estuary does not end sharply, as suggested
Journal Article
Journal: PALAIOS
Published: 01 December 2007
PALAIOS (2007) 22 (6): 691–694.
...JIAN HAN; ZHIFEI ZHANG; JIANNI LIU; DEGAN SHU Abstract A Laojieella specimen of the Lower Cambrian Chengjiang Lagerstätte in Yunnan Province, southern China, contains a tubular organism inside its digestive tract. The gut content appears to resemble Archotuba conoidalis , a sessile animal...
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First thumbnail for: EVIDENCE OF PRIAPULID SCAVENGING FROM THE EARLY CA...
Journal Article
Journal: Economic Geology
Published: 01 December 2023
Economic Geology (2023) 118 (8): 1857–1880.
...Wenbo Li; Fanghua Zhang; Xueyuan Qiao; Tianyao Fu Abstract Carbonaceous materials are a key factor controlling mineralization processes in many world-class gold deposits. Haoyaoerhudong is the largest carbonaceous metasediment-hosted gold deposit on the north margin of the North China craton. Gold...
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