Cretaceous anomalous subsidence and its response to dynamic topography in the Songliao Basin, Northeast China

Li, Chao; Liu, Shaofeng

doi:10.1016/j.jseaes.2015.04.045

Cited by 31 publications

(17 citation statements)

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“…Cretaceous basins in northeast Asia (Feng et al, 2010;Li and Liu, 2015). We found that the predicted post-rift subsidence that was based on the uniform stretching model that followed earlier lithospheric thinning events was much lower than the subsidence that was provided by back stripping.…”

Section: Accepted Manuscript 10 2009mentioning

confidence: 61%

“…We found that the predicted post-rift subsidence that was based on the uniform stretching model that followed earlier lithospheric thinning events was much lower than the subsidence that was provided by back stripping. The residual subsidence, i.e., the difference between the modelled and observed (or back-stripped) subsidence, during the post-rift stage was between 200 m and 800 m (Li and Liu, 2015). This regional residual subsidence suggests a possible deficit in the negative buoyancy (mantle loading) that was induced by downward drag pressure from the subducting western Izanagi slab and asthenospheric mantle flow beneath the Songliao basin, which was similar to what occurred in the Western Interior Seaway basin of the United States (Liu and Nummedal, 2004;Liu et al, 2014).…”

Section: Accepted Manuscript 10 2009mentioning

confidence: 99%

“…100 Ma (Li and Liu 2015). We believe that this lack of thermal subsidence in the Cretaceous rift basins was caused by anomalous uplift (minimal anomalous uplift) between ca.…”

mentioning

confidence: 92%

“…We believe that this lack of thermal subsidence in the Cretaceous rift basins was caused by anomalous uplift (minimal anomalous uplift) between ca. 300 m and 400 m according to the results of a 1D strain rate inversion model (Li and Liu, 2015).…”

mentioning

confidence: 99%

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Reconstruction of northeast Asian deformation integrated with western Pacific plate subduction since 200 Ma

Liu

Gurnis

et al. 2017

Earth-Science Reviews

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The configuration and kinematics of continental deformation and its marginal plate tectonics on the Earth's surface are intrinsic manifestations of plate-mantle coupling. The complex interactions of plate boundary forces result in plate motions that are dominated by slab pull and ridge push forces and the effects of mantle drag; these interactions also result in continental deformation with a complex basin-mountain architecture and evolution. The kinematics and evolution of the

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Section: Accepted Manuscript 10 2009mentioning

confidence: 61%

Section: Accepted Manuscript 10 2009mentioning

confidence: 99%

“…100 Ma (Li and Liu 2015). We believe that this lack of thermal subsidence in the Cretaceous rift basins was caused by anomalous uplift (minimal anomalous uplift) between ca.…”

mentioning

confidence: 92%

mentioning

confidence: 99%

See 2 more Smart Citations

Reconstruction of northeast Asian deformation integrated with western Pacific plate subduction since 200 Ma

Liu

Gurnis

et al. 2017

Earth-Science Reviews

Self Cite

200

134

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“…This regional event was synchronous with significant crustal downflexing and loading, and accommodation‐space development in the Songliao basin. Detailed studies of the stratigraphy and sedimentology of the Songliao basin have shown that subsidence rates in this depozone were anomalously accelerated during its post‐rift evolution in the late Cretaceous (Li & Liu, ). This mode of subsidence differs from the overall decay patterns of post‐rift subsidence observed in individual extensional sedimentary basins (Allen & Allen, ).…”

Section: Delineation Of a Late Cretaceous Retroarc Foreland Basin In mentioning

confidence: 99%

Late Cretaceous tectonic switch from a Western Pacific‐ to an Andean‐Type continental margin evolution in East Asia, and a foreland basin development in NE China

et al. 2017

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The early Cretaceous structure of NE China was a result of slab‐rollback‐driven extensional tectonics, characteristic of Western Pacific‐type continental margins. Oblique docking of a microcontinent along the Asian active margin in the early Late Cretaceous induced a compressional stress regime that brought about an Andean‐type continental margin development. Partitioning of contractional–transpressional strain across NE China produced a retroarc foreland basin system, comprising, from east to west, an orogenic wedge, a foredeep (Songliao basin), a forebulge (Great Xing'an Range) and a back‐bulge depozone (Hailar and Erlian basins). A sub‐circular lacustrine depozone in the pre‐existing Songliao basin evolved into a NNE‐trending depocentre near the forebulge and acquired a westward flowing fluvial–deltaic drainage system during the Campanian. Development of this retroarc foreland basin system signals a significant tectonic switch from a Western Pacific‐type to an Andean‐type continental margin evolution in the geological history of East Asia.

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Dawsonite occurrences related to the age and origin of CO₂ influx in sandstone reservoirs: A case study in the Songliao Basin, NEChina

Yu³

et al. 2017

Geochem Geophys Geosyst

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Dawsonite is often associated with CO 2 -rich gas reservoirs, and it is regarded as a ''trace mineral'' for recording migration and accumulation of CO 2 . Following accepted petrological, mineralogical, and geochemical principles, we used several methods (described herein) to study the Cretaceous dawsonitebearing sandstone reservoirs in the Songliao Basin, China. We used the ideas of ''sequencing'' and ''timing'' to verify the influx stages of CO 2 and hydrocarbons, dividing their influx sequence pattern and building a CO 2 -influx timeframe. First, we determined the stable isotopic ratios of dawsonite and CO 2 in gas and oil reservoirs, and found that the CO 2 in? dawsonite is of a mantle-derived magma origin. Second, we differentiated an early/late-stage oil and gas influx and a midmantle source influx through the study of diagenetic paragenetic sequences, formation water, and fluid inclusions in the dawsonite-bearing sandstones. Combining burial/thermal-history curves and illite K-Ar dates from the study area, we determined that the earlystage oil and gas influx, late oil and gas influx, and medium CO 2 influx occurred at Ma (Paleocene and Eocene), respectively. Finally, we observed a coupling relationship between CO 2 influx and Shuangliao volcanic activities and material compositions, as constrained by volcanic activity history in the basin since the Late Cretaceous.

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Cretaceous anomalous subsidence and its response to dynamic topography in the Songliao Basin, Northeast China

Cited by 31 publications

References 50 publications

Reconstruction of northeast Asian deformation integrated with western Pacific plate subduction since 200 Ma

Reconstruction of northeast Asian deformation integrated with western Pacific plate subduction since 200 Ma

Late Cretaceous tectonic switch from a Western Pacific‐ to an Andean‐Type continental margin evolution in East Asia, and a foreland basin development in NE China

Dawsonite occurrences related to the age and origin of CO₂ influx in sandstone reservoirs: A case study in the Songliao Basin, NEChina

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Cretaceous anomalous subsidence and its response to dynamic topography in the Songliao Basin, Northeast China

Cited by 31 publications

References 50 publications

Reconstruction of northeast Asian deformation integrated with western Pacific plate subduction since 200 Ma

Reconstruction of northeast Asian deformation integrated with western Pacific plate subduction since 200 Ma

Late Cretaceous tectonic switch from a Western Pacific‐ to an Andean‐Type continental margin evolution in East Asia, and a foreland basin development in NE China

Dawsonite occurrences related to the age and origin of CO2 influx in sandstone reservoirs: A case study in the Songliao Basin, NEChina

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Dawsonite occurrences related to the age and origin of CO₂ influx in sandstone reservoirs: A case study in the Songliao Basin, NEChina