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East China rift system

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Journal Article

HEAT FLOW IN CENOZOIC RIFTS IN EAST CHINA Available to Purchase

S.V. Lysak, R.P. Dorofeeva
Published: 01 June 2005
Russ. Geol. Geophys. (2005) 46 (6): 667–680.
...S.V. Lysak; R.P. Dorofeeva Heat flows in continental East China, which includes four Cenozoic rifts that belong to the western or eastern rift systems, vary from 26 to 106 mW/m 2 , with the mean of 61±2 mW/m 2 . The rifts are generally hotter than their surroundings (the mean of 68–70 mW/m 2...
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View PDF for article title, HEAT FLOW IN CENOZOIC <span class="search-highlight">RIFTS</span> IN <span class="search-highlight">EAST</span> <span class="search-highlight">CHINA</span>
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Journal Article

Detrital zircon records of late Paleoproterozoic to early Neoproterozoic northern North China Craton drainage reorganization: Implications for supercontinent cycles Available to Purchase

Chaohui Liu, Guochun Zhao, Fulai Liu, Jianrong Shi, Lei Ji
Journal: GSA Bulletin
Published: 09 March 2020
GSA Bulletin (2020) 132 (9-10): 2135–2153.
DOI: https://doi.org/10.1130/B35506.1
... rift-related magmatic products. Such a transition implies establishment of east–west drainage systems traversing the Paleoproterozoic Trans–North China Orogen caused by continued rifting since Statherian and pre-magmatic uplift during breakup of the North China Craton from the Columbia supercontinent...
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View PDF for article title, Detrital zircon records of late Paleoproterozoic to early Neoproterozoic northern North <span class="search-highlight">China</span> Craton drainage reorganization: Implications for supercontinent cycles
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Simplified map showing distribution of Cenozoic rifting systems and basalts in the Sino-Korean craton (SKC), eastern China (modified after Xu 2002). Note that the SKC is cut by two major geological and geophysical linear zones: the Tan-Lu fault zone (TLFZ) to the east and the Daxin'anling-Taihang gravity lineament (DTGL) to the west. Two rift systems (Yinchuan-Hetao and Shaanxi-Shanxi) occur in the western SKC. The North China rift system is located in the eastern SKC. Two shaded and dashed lines outline the central zone that separates the western and eastern zones of the SKC (after Zhao et al. 2001).

Simplified map showing distribution of Cenozoic rifting systems and basalts... Available to Purchase

Published: 01 September 2004
Figure 1. Simplified map showing distribution of Cenozoic rifting systems and basalts in the Sino-Korean craton (SKC), eastern China (modified after Xu 2002 ). Note that the SKC is cut by two major geological and geophysical linear zones: the Tan-Lu fault zone (TLFZ) to the east
Journal Article

Sedimentology, geochronology, and provenance of the late Cenozoic “Yangtze Gravel”: Implications for Lower Yangtze River reorganization and tectonic evolution in southeast China Available to Purchase

Ping Wang, Hongbo Zheng, Yongdong Wang, Xiaochun Wei, Lingyu Tang, Fred Jourdan, Jun Chen, Xiangtong Huang
Journal: GSA Bulletin
Published: 15 June 2021
GSA Bulletin (2022) 134 (1-2): 463–486.
DOI: https://doi.org/10.1130/B35851.1
... and local sources. From late Oligocene to early-middle Miocene, the post-rift subsidence opens a path for the ancient Lower Yangtze River connecting the Jianghan Basin, North Jiangsu-South Yellow Sea Basin, and East China Sea Shelf Basin. We attribute the drainage reorganization of the Lower Yangtze River...
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View PDF for article title, Sedimentology, geochronology, and provenance of the late Cenozoic “Yangtze Gravel”: Implications for Lower Yangtze River reorganization and tectonic evolution in southeast <span class="search-highlight">China</span>
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Journal Article

Balkatach hypothesis: A new model for the evolution of the Pacific, Tethyan, and Paleo-Asian oceanic domains Open Access

Andrew V. Zuza, An Yin
Journal: Geosphere
Published: 11 September 2017
Geosphere (2017) 13 (5): 1664–1712.
DOI: https://doi.org/10.1130/GES01463.1
... not a single well-defined belt, but rather a complex accretionary system of arcs and microcontinents. This immense collage is currently bounded to the north and south by the Siberia and North China–Tarim cratons, respectively, and extends from the Urals and Baltica in the west to the Pacific Ocean in the east...
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