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Large-scale climatic fluctuations in the latest Ordovician on the Yangtze block, south China

Geology (Boulder), 2010-07, Vol.38 (7), p.599-602

2010

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Lithofacies and depositional mechanisms of the Ordovician–Silurian Wufeng–Longmaxi organic-rich shales in the Upper Yangtze area, southern China

AAPG bulletin, 2020-01, Vol.103 (1), p.97-129

2020

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A study of the gas–water characteristics and their implications for the coalbed methane accumulation modes in the Southern Junggar Basin, China

AAPG bulletin, 2021-01, Vol.105 (1), p.189-221

2021

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A study of hydrogeology and its effect on coalbed methane enrichment in the southern Junggar Basin, China

AAPG bulletin, 2019-01, Vol.103 (1), p.189-213

2019

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Environmental conditions and mechanisms restricting microbial methanogenesis in the Miquan region of the southern Junggar Basin, NW China

Geological Society of America bulletin, 2023-01, Vol.135 (1-2), p.420-434

2023

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Volcanism-induced late Boda warming in the Late Ordovician: Evidence from the Upper Yangtze Platform, South China

Palaeogeography, palaeoclimatology, palaeoecology, 2021-09, Vol.578, p.110579, Article 110579

2021

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Volcanic and hydrothermal activities recorded in phosphate nodules from the Lower Cambrian Niutitang Formation black shales in South China

Palaeogeography, palaeoclimatology, palaeoecology, 2018-09, Vol.505, p.381-397

2018

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Anomalous weathering trends during the Early Silurian warming: Implications for the biotic crisis and recovery

Palaeogeography, palaeoclimatology, palaeoecology, 2023-12, Vol.632, p.111859, Article 111859

2023

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Evolution from an anoxic to oxic deep ocean during the Ediacaran–Cambrian transition and implications for bioradiation

Chemical geology, 2012-05, Vol.306-307, p.129-138

2012

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New U-Pb zircon ages of the Ediacaran-Cambrian boundary strata in South China

Terra nova (Oxford, England), 2015-02, Vol.27 (1), p.62-68

2015

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Implications of the pore pressure and in situ stress for the coalbed methane exploration in the southern Junggar Basin, China

Engineering geology, 2019-11, Vol.262, p.105305, Article 105305

2019

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Detrital zircon geochronology and heavy mineral composition constraints on provenance evolution in the western Pearl River Mouth basin, northern south China sea: A source to sink approach

Marine and petroleum geology, 2022-11, Vol.145, p.105884, Article 105884

2022

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Hydrothermal venting activities in the Early Cambrian, South China: Petrological, geochronological and stable isotopic constraints

Chemical geology, 2009-01, Vol.258 (3), p.168-181

2009

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Differential deformation on two sides of Qiyueshan Fault along the eastern margin of Sichuan Basin, China, and its influence on shale gas preservation

Marine and petroleum geology, 2020-11, Vol.121, p.104602, Article 104602

2020

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Abrupt change of pore system in lacustrine shales at oil- and gas-maturity during catagenesis

International journal of coal geology, 2020-08, Vol.228, p.103557, Article 103557

2020

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Pyrite Concretions in the Lower Cambrian Niutitang Formation, South China: Response to Hydrothermal Activity

Journal of earth science (Wuhan, China), 2023-08, Vol.34 (4), p.1053-1067

2023

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Insights into Pore Structure and Fractal Characteristics of the Lower Cambrian Niutitang Formation Shale on the Yangtze Platform, South China

Journal of earth science (Wuhan, China), 2020-02, Vol.31 (1), p.169-180

2020

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Geochemical and petrophysical characterization of potential gas shale reservoirs in the Lishu depression, southern Songliao Basin, northeastern China

AAPG bulletin, 2024-09, Vol.108 (9), p.1799-1826

2024

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Predominance of stratified anoxic Yangtze Sea interrupted by short-term oxygenation during the Ordo-Silurian transition

Chemical geology, 2012-01, Vol.291 (6), p.69-78

2012

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Stratigraphic framework, redox history, and organic matter accumulation of an Early Cambrian intraplatfrom basin on the Yangtze Platform, South China

Marine and petroleum geology, 2021-08, Vol.130, p.105095, Article 105095

2021

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Guadalupian (Middle Permian) ocean redox evolution in South China and its implications for mass extinction

Chemical geology, 2019-12, Vol.530, p.119318, Article 119318

2019

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Geochemical and petrographic characteristics of Wufeng-Longmaxi shales, Jiaoshiba area, southwest China: Implications for organic matter differential accumulation

Marine and petroleum geology, 2019-04, Vol.102, p.138-154

2019

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Oceanic environment changes caused the Late Ordovician extinction; evidence from geochemical and Nd isotopic composition in the Yangtze area, south China

Geological magazine, 2020-04, Vol.157 (4), p.651-665

2020

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Pore Structure and Multi-Scale Fractal Characteristics of Adsorbed Pores in Marine Shale: A Case Study of the Lower Silurian Longmaxi Shale in the Sichuan Basin, China

Journal of earth science (Wuhan, China), 2022-10, Vol.33 (5), p.1278-1290

2022

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Oceanic anoxia and extinction in the latest Ordovician

Earth and planetary science letters, 2022-06, Vol.588, p.117553, Article 117553

2022

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Large-scale climatic fluctuations in the latest Ordovician on the Yangtze block, south China

Lithofacies and depositional mechanisms of the Ordovician–Silurian Wufeng–Longmaxi organic-rich shales in the Upper Yangtze area, southern China

A study of the gas–water characteristics and their implications for the coalbed methane accumulation modes in the Southern Junggar Basin, China

A study of hydrogeology and its effect on coalbed methane enrichment in the southern Junggar Basin, China

Environmental conditions and mechanisms restricting microbial methanogenesis in the Miquan region of the southern Junggar Basin, NW China

Volcanism-induced late Boda warming in the Late Ordovician: Evidence from the Upper Yangtze Platform, South China

Volcanic and hydrothermal activities recorded in phosphate nodules from the Lower Cambrian Niutitang Formation black shales in South China

Anomalous weathering trends during the Early Silurian warming: Implications for the biotic crisis and recovery

Evolution from an anoxic to oxic deep ocean during the Ediacaran–Cambrian transition and implications for bioradiation

New U-Pb zircon ages of the Ediacaran-Cambrian boundary strata in South China

Implications of the pore pressure and in situ stress for the coalbed methane exploration in the southern Junggar Basin, China

Detrital zircon geochronology and heavy mineral composition constraints on provenance evolution in the western Pearl River Mouth basin, northern south China sea: A source to sink approach

Hydrothermal venting activities in the Early Cambrian, South China: Petrological, geochronological and stable isotopic constraints

Differential deformation on two sides of Qiyueshan Fault along the eastern margin of Sichuan Basin, China, and its influence on shale gas preservation

Abrupt change of pore system in lacustrine shales at oil- and gas-maturity during catagenesis

Pyrite Concretions in the Lower Cambrian Niutitang Formation, South China: Response to Hydrothermal Activity

Insights into Pore Structure and Fractal Characteristics of the Lower Cambrian Niutitang Formation Shale on the Yangtze Platform, South China

Geochemical and petrophysical characterization of potential gas shale reservoirs in the Lishu depression, southern Songliao Basin, northeastern China

Predominance of stratified anoxic Yangtze Sea interrupted by short-term oxygenation during the Ordo-Silurian transition

Stratigraphic framework, redox history, and organic matter accumulation of an Early Cambrian intraplatfrom basin on the Yangtze Platform, South China

Guadalupian (Middle Permian) ocean redox evolution in South China and its implications for mass extinction

Geochemical and petrographic characteristics of Wufeng-Longmaxi shales, Jiaoshiba area, southwest China: Implications for organic matter differential accumulation

Oceanic environment changes caused the Late Ordovician extinction; evidence from geochemical and Nd isotopic composition in the Yangtze area, south China

Pore Structure and Multi-Scale Fractal Characteristics of Adsorbed Pores in Marine Shale: A Case Study of the Lower Silurian Longmaxi Shale in the Sichuan Basin, China

Oceanic anoxia and extinction in the latest Ordovician

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