Middle Permian brachiopods from the Tumenling Formation in the Wuchang area, southern Heilongjiang, NE China, and their palaeobiogeographical implications

Tazawa, Jun-ichi; Chen, Zhong‐Qiang

doi:10.1016/j.jseaes.2005.06.008

Cited by 12 publications

(2 citation statements)

References 23 publications

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“…The studies by Tazawa and Chen (2005) on the brachiopods of the Tumenling Formation (Wordian-Capitanian) in the Wuchang area in the southern Heilongjiang Province of northern China document the unity of the northern part of the bridge already in the later medial Permian time. The Wuchang brachiopod fauna, as a whole, is found by them to be comparable to several contemporaneous faunas described from Inner Mongolia in northern China, Jilin in northeast China, south Primorye in eastern Russia, and the Hida Gaien belt of Japan (i.e., the old, pre-Permian nucleus of Japan: see Şengör and Natal'in, 1996, for its paleogeographic relation to the other areas here mentioned), in terms of its index elements and its boreal-paleoequatorial mixture.…”

Section: The Tectonics Of Pangea and The Paleo-tethys During The Latementioning

confidence: 99%

“…The overwhelming majority of the boreal elements reveal that the Wuchang area was probably situated in the northern subzone of this transitional zone, which belongs to the Manchurides, i.e., to the north China block. These east and northeast Asian blocks acted as migratory stepping stones providing a bridge for faunal migration between the paleoequatorial and boreal realms during the medial Permian (Tazawa and Chen, 2005).…”

Section: The Tectonics Of Pangea and The Paleo-tethys During The Latementioning

confidence: 99%

See 1 more Smart Citation

The Permian Extinction and the Tethys: An Exercise in Global Geology

Şengör¹,

Atayman²

2009

The Permian Extinction and the Tethys: An Exercise in Global Geology

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Section: The Tectonics Of Pangea and The Paleo-tethys During The Latementioning

confidence: 99%

Section: The Tectonics Of Pangea and The Paleo-tethys During The Latementioning

confidence: 99%

The Permian Extinction and the Tethys: An Exercise in Global Geology

Şengör¹,

Atayman²

2009

The Permian Extinction and the Tethys: An Exercise in Global Geology

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Hydrocarbon potential of Late Palaeozoic residual basins in the Central Asian Orogenic Belt: Insights from the tectonic evolution of the Yinggen‐Ejinaqi Basin, Inner Mongolia, China

Abitkazy

Shi

et al. 2019

Geological Journal

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The Yinggen‐Ejinaqi Basin (YEB) is located in the central‐southern part of the Central Asian Orogenic Belt (CAOB). Tectonically, the basin is situated at the intersection between the eastern and western CAOB, where Late Palaeozoic strata were well exposed. Hence, it offers a great opportunity to study the deep strata of the eastern CAOB. In this paper, based on extensive studies of Upper Palaeozoic field outcrops and reanalysis of associated geochemical and geochronological data in previous research, the local stratigraphic correlation is established, and the tectonic evolution, sedimentary filling, sedimentary characteristics, and petroleum system of the YEB are discussed. It is revealed that: (a) The filling characteristics of the Upper Palaeozoic strata in YEB are closely related to the closure of the Paleo‐Asian Ocean (PAO). YEB underwent subduction‐related compression during the initial extensional phase of the fore‐arc basin from the Viséan to the Serpukhovian (late Early Carboniferous). During the Bashkirian–Sakmarian interval (Late Carboniferous to Early Permian), it was in subduction‐related fore‐arc and postarc rifting phases. During the Artinskian–Capitanian (Early‐Middle Permian) times, it was in an intracontinental rifting‐depression phase. During the Wuchapingian (Late Permian), it was in an intracontinental compressional phase. Tectonostratigraphy, tectonic evolution, and hydrocarbon potential assessments of the study area show that the Zhusileng Hangwula‐Tost Ul tectonic zone (ZHTUTZ) and southwestern part of Querrshan‐Atasbogd tectonic zone (QATZ) are identified as the main prospective areas for the exploration in the YEB. (b) According to the tectonostratigraphic analysis, tectonic evolution and hydrocarbon system of Carboniferous–Permian in the YEB, the YEB has similar attributes to the basin province in western CAOB (e.g., Santanghu and Junggar basins) and eastern CAOB (Erlian, Songliao Basin). To explore commercial oil and gas in the deeper strata (Carboniferous–Permian) of the eastern CAOB basins, further tectonostratigraphic analyses and comprehensive assessment on hydrocarbon potentials are necessitated in the near future.

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Coevolution of brachiopod paleobiogeography and tectonopaleogeography during the late Paleozoic in Central Asia

Wang

Zhao

et al. 2013

Sci. China Earth Sci.

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Middle Permian brachiopods from the Tumenling Formation in the Wuchang area, southern Heilongjiang, NE China, and their palaeobiogeographical implications

Cited by 12 publications

References 23 publications

The Permian Extinction and the Tethys: An Exercise in Global Geology

The Permian Extinction and the Tethys: An Exercise in Global Geology

Hydrocarbon potential of Late Palaeozoic residual basins in the Central Asian Orogenic Belt: Insights from the tectonic evolution of the Yinggen‐Ejinaqi Basin, Inner Mongolia, China

Coevolution of brachiopod paleobiogeography and tectonopaleogeography during the late Paleozoic in Central Asia

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