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Maidiping Formation

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Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping (sample No begins with MD2), Yushan (sample No begins with MDP) and Daqiao Mine (sample No begins with GWS3) sections, South Sichuan, China. (a–d), Rugatotheca typica He in Yin et al., 1980, (a, b) No GWS301-04. (a), longitudinal view; (b), transversal view. (c, d), No MD241_008. (c), longitudinal view; (d), transversal view. (e–j), Coleolella recta (Mambetov in Missarzhevsky and Mambetov, 1981). (e), lateral view, No MD240-005; (f), transversal view. (g), longitudinal view, No MDP100_12; (h), transversal view. (i), transversal view, No MDP100_10; (j), longitudinal view. (k), Cloudina cf. hartmannae Germs, 1972, longitudinal view, No MD241_021. (l), A gregarious cluster of undetermined algae (Girvanella?), No MDP100-02. (m, n), Arthrochites emeishanensis Chen, 1982, No MD241-002. (m), lateral view; (n), proximal view. (o), Olivooides sp., lateral view, No GWS301-01. (p), Olivooides multisulcatus Qian, 1977, No GWS301-11. (q, r), Maikhanella cambrina (Jiang in Luo et al., 1982), No MDP100-07. (q), distal view; (r), lateral view. (s, t), Spirellus columnaris Jiang in Luo et al., 1982, No MDP100-05. (s), lateral view; (t), proximal view. Scale bars: (a, c, d, j, p–r), 200 μm; others 100 μm.
Published: 13 April 2021
Fig. 5 Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping (sample No begins with MD2), Yushan (sample No begins with MDP) and Daqiao Mine (sample No begins with GWS3) sections, South Sichuan, China. ( a – d ), Rugatotheca typica He in Yin et al. , 1980 , ( a, b
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Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping (sample No begins with MD) and Yushan (sample No begins with MDP) and Daqiao Mine (sample No begins with GWS3) sections, Gaoqiao Town, Emei City of Sichuan Province, China. (a, b), Quadrosiphogonuchites curvatornatus Chen, 1982, No MD241-017. (a), lateral view; (b), proximal view. (c, d), Quadrosiphogonuchites antiquus Chen, 1982, No MD241-028. (c), lateral view; (d), proximal view. (e, f), Quadrosiphogonuchites quadratus, Chen, 1982, No MD241-030. (e), lateral view; (f), proximal view. (g), Olivooides multisulcatus Qian, 1977, No MD226-012. (h), Aetholicopalla adnata Bengtson et al., 1990, No MDP123-009. (i, j), Cupitheca mira (He in Qian, 1977), No MD235-015. (i), lateral view; (j), transversal view. (k, l), Paragloborilus subglobosus He in Qian, 1977, No MD228-002. (m, n), Pseudovalitheca crassa Yu, 1974, No MD237-002. (m), lateral view; (n), transversal view. (o, p), Halkieria sthenobasis Jiang in Luo et al., 1982, No MD228-012. (o), Lateral view; (p), proximal view. (q, r), Siphogonuchites triangularis Qian, 1977, No MDP123-017. (q), lateral view; (r), proximal view. (s, t), Lomasulcachites macrus Qian and Jiang in Luo et al., 1982. (s), lateral view; (t), transversal view. Scale bars: (c, d, f, h), 100 μm; others 200 μm.
Published: 13 April 2021
Fig. 6 Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping (sample No begins with MD) and Yushan (sample No begins with MDP) and Daqiao Mine (sample No begins with GWS3) sections, Gaoqiao Town, Emei City of Sichuan Province, China. ( a , b ), Quadrosiphogonuchites
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Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping section, Gaoqiao Town, Emei City of Sichuan Province. (a–c), Maikhanella cf. cambrina (Jiang in Luo, et al. 1982), No MD235-001; (a) distal view; (b) front view; (c) lateral view. (d–f) Maikhanellalatispina (Feng, et al. 2001), No MD239-007; (d) distal view; (e) lateral view; (f) front view. (g–k) Purella elegans (Yu, 1979); (g) distal view, No MD235-016; (h) lateral view; (i) front view; (j) distal view, No MD117_01; (k) lateral view. (l, m) Oelandiella korobkovi Vostokova, 1962, No MD117_11; (l) lateral view; (m) distal view. (n–p), Lathamella caeca Liu, 1979, No MD116-05; (n) distal view; (o) lateral view; (p) front view. (q–s) Codonoconus sinensis Chen and Zhang, 1980, No MD230-001; (q) front view; (r) distal view; (s) lateral view. (t, u) Aegitellus emeishanensis (He in Yin et al., 1980), No MD230-008; (t) lateral view; (u) distal view. Scale bars: (l, m) 500 μm; others 200 μm.
Published: 13 April 2021
Fig. 7 Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping section, Gaoqiao Town, Emei City of Sichuan Province. ( a – c ), Maikhanella cf. cambrina (Jiang in Luo, et al. 1982 ), No MD235-001; ( a ) distal view; ( b ) front view; ( c ) lateral view. ( d – f
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Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping section, Gaoqiao Town, Emei City of Sichuan Province, China. (a–c) Ocruranus finial Liu, 1979, No MD235-011; (a) distal view; (b) lateral view; (c) front view. (d–f) Eohalobia diandongensis Jiang, in Luo et al., 1982, No MD116_007; (d) distal view; (e) front view; (f) lateral view. (g–i) Bemella simplex Yu, 1979, No MD228-013; (g) distal view; (h) lateral view; (i) front view. (j–l) Obtusoconus rostriptuetus (Qian, 1978), No MD117_17; (j) distal view; (k, l) lateral view. (m–o) Acutirostriconus simplex Yue in Xing et al., 1984, No MD239-013; (m) lateral view; (n) distal view; (o) front view. (p–r) Protoconus crestatus Yu, 1979, No MD235-013; (p) distal view; (q) lateral view; (r) front view. (s–u), Bemella minuta Jiang in Luo et al., 1982, No MD228-006; (s) distal view; (t) front view; (u) lateral view. (v–z) Undetermined fossils; (v) lateral view, No MD116-03; (w) front view; (x) distal view. (y) distal view, No MD116-10; (z) lateral view. Scale bars: (a–c, m–o) 100 μm; others 200 μm.
Published: 13 April 2021
Fig. 8 Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping section, Gaoqiao Town, Emei City of Sichuan Province, China. ( a – c ) Ocruranus finial   Liu, 1979 , No MD235-011; ( a ) distal view; ( b ) lateral view; ( c ) front view. ( d – f ) Eohalobia diandongensis
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Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping section, Gaoqiao Town, Emei City of Sichuan Province, China. (a–c) Zhijinites longistriatus Qian, 1978, No MD230-013; (a, b) lateral view; (c) distal view. (d, e), Lopochites latazonalis Qian, 1977, MD228_018; (d) lateral view; (e) proximal view. (f, g) Brushenodus prionnodes (Luo et al., 1982), No MD239-004; (f) lateral view; (g) proximal view. (h–j) Paracarinachites sinensis Qian and Jiang in Luo et al., 1982, No MD230-002; (h) distal view; (i) lateral view; (j) distal view. (k, l) Lopochites cf. latazonalis Qian, 1977, No MD239-020; (k) distal view; (l) lateral view. (m, n) Chancelloria symmetrica Vassiljeva, 1985, No MD235-014; (m) distal view; (n) proximal view showing pits around the basal foramina. (o–q) Kuanchuanella sp., No MD228-017; (o) lateral view; (p) distal view; (q) proximal view. (r, s) Emarginoconus mirus Yu, 1979, No MD230-005; (r) lateral view; (s) distal view. (t–v) Watsonella crosbyi Grabau, 1900, No MD239-001; (t) front view; (u) dorsal view; (v) lateral view. Scale bars: (k, l, n) 100 μm; others 200 μm.
Published: 13 April 2021
Fig. 9 Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping section, Gaoqiao Town, Emei City of Sichuan Province, China. ( a – c ) Zhijinites longistriatus   Qian, 1978 , No MD230-013; ( a , b ) lateral view; ( c ) distal view. ( d , e ), Lopochites latazonalis
Journal Article
Published: 13 April 2021
Journal of the Geological Society (2021) 178 (5): jgs2020-167.
...Fig. 5 Terreneuvian small shelly fossils from the Maidiping Formation at the Maidiping (sample No begins with MD2), Yushan (sample No begins with MDP) and Daqiao Mine (sample No begins with GWS3) sections, South Sichuan, China. ( a – d ), Rugatotheca typica He in Yin et al. , 1980 , ( a, b...
FIGURES | View All (10)
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Representative outcrop photographs of the Lower Cambrian at the Longzikou section, Beichuan County. (a) Black thin-bedded siliceous shale from the lower Maidiping Formation. (b) Interbedded thin dolomite and chert from the lower Maidiping Formation. (c) Black thin-bedded siliceous shale with pyrite nodules in the upper part of the Maidiping Formation. (d) A volcanic ash bed interlayered with black shale in the Qiongzhusi Formation. (e) A medium limestone bed interlayered with thin-bedded mudstone, in the upper part of the Canglangpu Formation. (f) Thin to medium siltstone, in the middle Canglangpu Formation, showing a small-scale coarsening-upward sequence. (g) Current ripples from the sandstone in the middle Canglangpu Formation showing a SE-vergent palaeocurrent direction (oriented at 120°). (h) Thick coarse-grained sandstone with minor conglomerate in the upper Canglangpu Formation.
Published: 05 May 2023
Fig. 6. Representative outcrop photographs of the Lower Cambrian at the Longzikou section, Beichuan County. ( a ) Black thin-bedded siliceous shale from the lower Maidiping Formation. ( b ) Interbedded thin dolomite and chert from the lower Maidiping Formation. ( c ) Black thin-bedded siliceous
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Location of sections (a, b) and field photographs (c–g) of the Maidiping and Daqiao Mine sections in South Sichuan. (a) Location of sections and Sichuan Province on the Yangtze Platform (grey shading). The red box marks the area shown enlarged in (b). (b) Geographic location of the Maidiping and Daqiao Mine sections in Sichuan Province. (c) The lower phosphorite of the Maidiping Formation in an abandoned mining tunnel in the Madiping section (red arrow in (d)). (d) Overview of the Maidiping section. (e) Overview of the complementary section (Yushan section) about 0.5 km to the north of the Maidiping section. (f) Overview of the Daqiao Mine section in a mining tunnel showing phosphorite interlayered with dolostone overlying the Dengying Formation (base of the mining tunnel; marker pen for scale). (g) Close-up of the unconformity contact of the Dengying and Maidiping Formations in the Daqiao section; note the palaeo-karst veins (red arrows) filled with Cambrian dolomitic granular phosphorite reaching down within the greyish blocky dolostone of the Ediacaran Dengying Formation for up to 60 cm.
Published: 13 April 2021
of the Maidiping and Daqiao Mine sections in Sichuan Province. ( c ) The lower phosphorite of the Maidiping Formation in an abandoned mining tunnel in the Madiping section (red arrow in ( d )). ( d ) Overview of the Maidiping section. ( e ) Overview of the complementary section (Yushan section) about 0.5 km
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Stratigraphic column of the Yushan section near to the Maidiping section (a) and the Daqiao Mine section (b) with the distribution of early Cambrian small shelly fossils in the Maidiping Formation.
Published: 13 April 2021
Fig. 3 Stratigraphic column of the Yushan section near to the Maidiping section ( a ) and the Daqiao Mine section ( b ) with the distribution of early Cambrian small shelly fossils in the Maidiping Formation.
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Stratigraphic column of the Maidiping section with the δ13C values of carbonates and distribution of early Cambrian small shelly fossils in the Maidiping Formation. For the legend of the lithology see Figure 3.
Published: 13 April 2021
Fig. 2 Stratigraphic column of the Maidiping section with the δ 13 C values of carbonates and distribution of early Cambrian small shelly fossils in the Maidiping Formation. For the legend of the lithology see Figure 3 .
Journal Article
Published: 22 August 2024
Journal of the Geological Society (2024) 181 (6): jgs2023-231.
... that the Yangjiagou Member is provisionally equivalent to the Zhongyicun Member of Yunnan, the Yanjiahe Formation of Hubei, the Maidiping Formation of Sichuan and the Kuanchuanpu Formation of Shaanxi. This paper offers new evidence and fossil data for the location of the Precambrian–Cambrian boundary...
FIGURES | View All (12)
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Paleogeographic evolution map of the South China cratonic basin during the critical period. (A) Nanhua Datangpo Formation. (B) Ediacaran Doushantuo Formation. (C) Cambrian Maidiping Formation. (D) Cambrian Qiongzhusi Formation.
Published: 01 April 2025
Figure 7. Paleogeographic evolution map of the South China cratonic basin during the critical period. (A) Nanhua Datangpo Formation. (B) Ediacaran Doushantuo Formation. (C) Cambrian Maidiping Formation. (D) Cambrian Qiongzhusi Formation.
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Thickness contour map of key strata source rocks in South China cratonic basin. Modified from Zhu et al. (2023b) and Zhu et al. (2020b). (A) Nanhua Datangpo Formation. (B) Ediacaran Doushantuo Formation. (C) Cambrian Maidiping Formation. (D) Cambrian Qiongzhusi Formation.
Published: 01 April 2025
Figure 18. Thickness contour map of key strata source rocks in South China cratonic basin. Modified from Zhu et al. (2023b) and Zhu et al. (2020b) . (A) Nanhua Datangpo Formation. (B) Ediacaran Doushantuo Formation. (C) Cambrian Maidiping Formation. (D) Cambrian Qiongzhusi Formation.
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Upper continental crust (UCC) normalized element patterns of Maidiping Formation (a), Qiongzhusi Formation (b) and Canglangpu Formation (c) samples from the Longzikou section. UCC composition data are from Taylor and McLennan (1985).
Published: 05 May 2023
Fig. 11. Upper continental crust (UCC) normalized element patterns of Maidiping Formation ( a ), Qiongzhusi Formation ( b ) and Canglangpu Formation ( c ) samples from the Longzikou section. UCC composition data are from Taylor and McLennan (1985).
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Evolution model of the Deyang–Anyue intracratonic rift. 1, dolostone; 2, fault; 3, algal mound; 4, Dengyingzu Formation argillutite; 5, Maidiping Formation marl; 6, argillutite.
Published: 01 April 2020
Fig. 4. Evolution model of the Deyang–Anyue intracratonic rift. 1 , dolostone; 2 , fault; 3 , algal mound; 4 , Dengyingzu Formation argillutite; 5 , Maidiping Formation marl; 6 , argillutite.
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Histograms displaying concentrations (A) and relative percentages (B) of detrital, diagenetic, and other silica in studied samples of lower Cambrian (A) and lower Silurian (B) successions of the middle–upper Yangtze platform. MDP = Maidiping Formation; STJ/QZS = Shuijingtuo/Qiongzhusi Formations; WF-LMX = Wufeng–Longmaxi Formations.
Published: 01 June 2024
Figure 12. Histograms displaying concentrations (A) and relative percentages (B) of detrital, diagenetic, and other silica in studied samples of lower Cambrian (A) and lower Silurian (B) successions of the middle–upper Yangtze platform. MDP = Maidiping Formation; STJ/QZS = Shuijingtuo/Qiongzhusi
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Post-Archean average shale (PAAS)-normalized rare earth elements and Y values of three Maidiping Formation mudstone samples (high SiO2 and low Al2O3 concentrations; see Figure 11A) and North Pacific seawater (Alibo and Nozaki, 1999).
Published: 01 June 2024
Figure 13. Post-Archean average shale (PAAS)-normalized rare earth elements and Y values of three Maidiping Formation mudstone samples (high SiO 2 and low Al 2 O 3 concentrations; see Figure 11A ) and North Pacific seawater ( Alibo and Nozaki, 1999 ).
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Stratigraphic column of the upper Ediacaran–lower Silurian succession of the middle–upper Yangtze platform. The lithology nomenclature of fine-grained sedimentary rocks was cited from Lazar et al. (2015). Lithologies and thicknesses of various formations were cited from Zou et al. (2014). Ed. = Ediacaran; Fm. = Formation; GYQ = Guanyinqiao Member; MDP = Maidiping Formation; Upp. = Upper; YJH = Yanjiahe Formation.
Published: 01 June 2024
. (2014) . Ed. = Ediacaran; Fm. = Formation; GYQ = Guanyinqiao Member; MDP = Maidiping Formation; Upp. = Upper; YJH = Yanjiahe Formation.
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Carbon isotopic composition of gas within the Dengying reservoir and of samples from the five possible source rocks. Gas carbon isotopes are from Wei et al. (2014) and Luo et al. (2015). Z1ds = the Lower Doushantuo Formation; Z2dy = the Upper Dengying Formation; Z2dy3 = the third member of the Dengying Formation; Є1m = the Lower Cambrian Maidiping Formation; Є1q = the Lower Cambrian Qiongzhusi Formation.
Published: 01 May 2018
= the third member of the Dengying Formation; Є 1 m = the Lower Cambrian Maidiping Formation; Є 1 q = the Lower Cambrian Qiongzhusi Formation.
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Integrated outcrop-well-seismic deposition profile of the Dengying–Qiongzhusi Formations. 1, basement; 2, fault; 3, coarse clastic rift infill; 4, siliceous and phosphoric dolomitic mudstone; 5, mudstone; 6, silty mudstone; 7, argillaceous siltstone; 8, siltstone; 9, phosphoric dolostone; 10, slump deposits; 11, limy dolomite; 12, Qiongzhusi Formation; 13, Members 1, 2, and 4 of the Dengying Formation; 14, dolomite; 15, breccia dolomite; 16, siliceous dolomite; 17, argillaceous dolomite; 18, knobby dolomite; 19, limestone; 20, intraplatform beach; 21, platform-margin beach; 22, intraplatform mound; 23, platform-margin mound; 24, Maidiping Formation; 25, Member 3 of the Dengying Formation; 26, Doushantuo Formation.
Published: 01 April 2020
; 21 , platform-margin beach; 22 , intraplatform mound; 23 , platform-margin mound; 24 , Maidiping Formation; 25 , Member 3 of the Dengying Formation; 26 , Doushantuo Formation.