Cretaceous source to sink system reconstruction of northeastern Asian continental margin: Insight from integrated detrital geochronology in NE China

Jian-ping, Zhou; Dunkl, İstván; Liu, Yongjiang; Li, Sanzhong; Liu, Weimin; Eynatten, Hilmar von

doi:10.1016/j.gsf.2023.101616

Cited by 1 publication

(6 citation statements)

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“…(2017), and J. P. Zhou et al. (2023). The digital elevation maps from (b–g) represent the general uplift process of eastern NE Asia, modified from the current‐day topography.…”

Section: Discussionmentioning

confidence: 99%

“…To the east of the Songliao Basin, the Sanjiang Basin and its neighboring basins underwent compression and inversion processes. Resulting in the exhumation of basement highs, notably that with the exhumation of the JU, the large proto‐basin underwent destruction (e.g., Sha et al., 2008; F. Q. Zhang et al., 2012; J. P. Zhou et al., 2022, 2023). The Late Cretaceous cooling events from the shallow surface could thus be proposed as the synchronous basin‐and‐range changing response of the East Asian crust to the same underlying flat slab subduction.…”

Section: Discussionmentioning

confidence: 99%

“…The formation of satellite basins in eastern NE Asia is commonly attributed to multiple uplift events since the Early Cretaceous (X. Zhang & Ma, 2010; J. B. Zhou et al., 2009; J. P. Zhou et al., 2022, 2023). The current roughly east‐west trending basin‐bordering system is thought to have developed during the late Early Cretaceous‐Late Cretaceous (Han et al., 2008).…”

Section: Geological Backgroundmentioning

confidence: 99%

“…Furthermore, the satellite basins located to the east of the Songliao Basin are recognized as remnant basins, integral components of a vast proto‐basin known as the “pan‐Sanjiang” or “Great Sanjiang” Basin, which emerged during the Early Cretaceous and underwent progressive deconstruction since the early Late Cretaceous (Jia & Zheng, 2010; Wen et al., 2008; Y. P. Zhang et al., 2016; J. B. Zhou et al., 2009; J. P. Zhou et al., 2022, 2023).…”

Section: Introductionmentioning

confidence: 99%

“…(a-g), Schematic cartons for the tectonic evolution of eastern NE Asia since 200 Ma. The plate subduction modes are after S. Z. Li et al (2019), L. J. Liu et al (2021), Ma et al (2019), P. J. Wang et al (2016), Xu et al (2013), F. Q. Zhang et al (2017), and J. P Zhou et al (2023)…”

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confidence: 97%

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Differential Uplift Triggered Basin‐And‐Range System: Evidence From Low‐Temperature Thermochronology in Eastern NE Asia

Zhou,

Li,

Liu

et al. 2023

Tectonics

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Since the Mesozoic, eastern NE Asia has experienced multiple tectonic events, resulting in a complex structure and forming one of the world's largest Meso‐Cenozoic lacustrine basin systems. Presently, basin evolution models require further elucidation regarding the simultaneous generation of diverse rift basins and the potential impact stemming from the closure of the Mudanjiang Ocean, whose oceanic closure demarcated the boundary between the Songliao Basin and the eastern basins, raises questions about its influence on the development of the basin‐and‐range system. To address these questions, we augment new low‐temperature thermochronological data on basement highs separating the eastern NE Asia basins to investigate the shallow‐deep coupling process of tectonic evolution since the Mesozoic. The new cooling age pattern shows non‐overlapping and spatial differences among major basement highs. Inverse thermal modeling revealed five‐stage cooling episodes among the basement highs, but with different onset and cooling rates of each episode, indicating a significant differential uplift mode. A major reburial stage was identified throughout eastern NE Asia during the mid‐Cretaceous. Compiling cooling age patterns and inverse thermal modeling, we note the existence of a proto‐basin covering an area much larger than the previously contemplated “Pan‐Sanjiang” Basin. In general, our study indicates the final closure of the Mudanjiang Ocean occurred at ca. 150–140 Ma. Since the Early Cretaceous, with changes in the subduction direction, two‐stage flat slab subduction of the Paleo‐Pacific plate and the consequent subduction of the Pacific plate co‐dominated the basements' differential uplift and the formation of the eastern NE Asia basin‐and‐range framework.

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“…(2017), and J. P. Zhou et al. (2023). The digital elevation maps from (b–g) represent the general uplift process of eastern NE Asia, modified from the current‐day topography.…”

Section: Discussionmentioning

confidence: 99%

Section: Discussionmentioning

confidence: 99%

Section: Geological Backgroundmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

mentioning

confidence: 97%

See 3 more Smart Citations

Differential Uplift Triggered Basin‐And‐Range System: Evidence From Low‐Temperature Thermochronology in Eastern NE Asia

Zhou,

Li,

Liu

et al. 2023

Tectonics

Self Cite

View full text Add to dashboard Cite

show abstract

Cretaceous source to sink system reconstruction of northeastern Asian continental margin: Insight from integrated detrital geochronology in NE China

Cited by 1 publication

References 59 publications

Differential Uplift Triggered Basin‐And‐Range System: Evidence From Low‐Temperature Thermochronology in Eastern NE Asia

Differential Uplift Triggered Basin‐And‐Range System: Evidence From Low‐Temperature Thermochronology in Eastern NE Asia

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