杨生超

发布者:陆昀乔发布时间:2024-10-27浏览次数:1489

A. 第一作者/通讯作者论文

[1] Yang, S.C., Hu, W.X.*, Wang, X.L., et al., Duration, evolution, and implications of volcanic activity across the Ordovician–Silurian transition in the Lower Yangtze region, South China. Earth and Planetary Science Letters, 2019, 518, 13-25.

[2] Yang, S.C.,Fan, J.X.*, Algeo, T.J., et al., Steep oceanic DIC δ13Cdepth gradient during the Hirnantian Glaciation.  Earth-Science Reviews, 2024, 255, 104840. 

[3] Yang, S.C., Hu, W.X.*, Fan, J.X., et al., New geochemical identification fingerprints of volcanism during the Ordovician-Silurian transition and its implications for biological and environmental evolution. Earth-Science Reviews, 2022, 228, 104016.

[4] Yang, S.C., Hu, W.X.*, Fan, J.X., et al., Nitrogen isotope evidence for a redox-stratified ocean and eustatic fall driven environmental evolution during the Ordovician–Silurian transition. Global and Planetary Change, 2021, 207, 103682.

[5] Yang, S.C., Hu, W.X.*, Wang, X.L.,Evidences, mechanism and implications of widespread upwelling during the Late Ordovician to early Silurian in the Yangtze region, South China. Chemical Geology, 2021, 565, 120074.

[6] Yang, S.C., Hu, W.X.*, Yao, S.P., et al., Constraints on the accumulation of organic matter in Upper Ordovician-Lower Silurian black shales from the Lower Yangtze region, South China. Marine and petroleum geology, 2020, 120, 104544.

[7] Deng, Y.Y., Fan, J.X.*,Yang, S.C. (Co-first author)et al., No Furongian Biodiversity Gap: Evidence from South China.Palaeogeography, Palaeoclimatology, Palaeoecology, 2023, 618, 111492.

[8] Qiu, L.W.*, Yang, S.C.*(Co-corresponding author), Qu, C.S., et al., A Comprehensive Porosity Prediction Model for the Upper Paleozoic Tight Sandstone Reservoir in the Daniudi Gas Field, Ordos Basin. Journal of Earth Science, 2017, 28(6), 1086-1096. 

[9] 杨生超, 邱隆伟*, 徐宁宁, . 渤海湾盆地济阳坳陷邵家洼陷沙四段湖相碳酸盐岩储层特征与分类评价[J]. 天然气地球科学, 2016, 27(4): 628-638.

[10] 杨生超, 邱隆伟*, 刘魁元, . 邵家洼陷沙四段湖相碳酸盐岩岩性测井解释模型[J]. 新疆石油地质, 2015, 12(6): 708 -713.

[11] 连丽霞, 王剑, 马聪, 杨召, 罗正江, 杨生超*, . 准噶尔盆地西北缘沸石发育特征及成储机理初探以玛南地区二叠系乌尔禾组为例[J]. 高校地质学报2021, 27(1): 102-110.


B. 合作论文

[1] Sun, F., Hu, W., Wang, X., Cao, J., Fu, B., Wu, H., Yang, S.C., Methanogen microfossils and methanogenesis in Permian lake deposits. Geology, 2020, 48. G47857.1

[2] Sun, F., Hu, W., Wu, H., Fu, B., Wang, X., Tang, Y., Cao, J., Yang, S.C., et al., Two-stage mineral dissolution and precipitation related to organic matter degradation: Insights from in situ C–O isotopes of zoned carbonate cements. Marine and Petroleum Geology, 2021, 565, 104812.

[3] Zhang, W., Hu, W., Yang, S.C., et al., Differences and constraints of varying gas dryness coefficients in the Cainan oil-gas field, Junggar Basin, NW China. Marine and Petroleum Geology, 2022, 139, 105582.

[4] Li, J., Zhang, W., Xiang, B., He, D., Yang, S.C., et al., Characteristics of dissolved pores and dissolution mechanism of zeolite-rich reservoirs in the Wuerhe Formation in Mahu area, Junggar Basin. Energy Exploration & Exploitation, 2022, 40, 421-441.

[5] 邱隆伟, 贾继成, 马立驰, 杨勇强, 孙超, 辛也, 王鑫, 杨生超. 孤北洼陷长堤断裂带扇三角洲砂砾岩体沉积特征及空间展布规律[J]. 石油与天然气地质, 2018, 39(1): 175-182.

[6] 邱隆伟, 师政, 付大巍, 潘泽浩, 杨生超, . 临南洼陷沙三段孔隙度控制因素分析与定量模型[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1321-1331.

[7] 徐宁宁, 邱隆伟, 刘魁元, 杨生超, . 沾化凹陷渤南罗家地区沙四上亚段层序地层及沉积演化研究[J]. 地层学杂志, 2015, 39(2): 223-231.

[8] 邱隆伟, 徐宁宁, 刘魁元,杨生超, . 渤南洼陷沙四上亚段储层异常高孔带及优质储层成因机制[J]. 天然气地球科学, 2015, 26(1): 1-12.

[9] 邵雨, 杨勇强, 万敏, 邱隆伟, 操应长, 杨生超. 吉木萨尔凹陷二叠系芦草沟组沉积特征及沉积相演化[J]. 新疆石油地质, 2015, 36(6): 635-641.

[10] 徐宁宁, 邱隆伟, 杨生超, . 渤南断阶带沙四上亚段储层成岩演化研究[J]. 中国矿业大学学报, 2015, 44(1): 104-115.


C. 参加会议

[1Yang, S.C., 2024/09. GSA Connects 2024 meeting, Anaheim, California, USA. 口头报告.

[2Yang, S.C., 2024/08. The 37th International Geological Congress, Busan, Korea. 口头报告.

[3杨生超, 樊隽轩, Thomas J. Algeo, 李超, 沈树忠. 奥陶纪末生物大灭绝期间广泛的分层海洋结构. 2023/11. 中国古生物学会第十三次会员代表大会暨第31届学术年会, 南京. 口头报告.


担任多家学术期刊审稿人,包括Global and Planetary Change, Marine and Petroleum Geology, Palaeogeography, Palaeoclimatology, Palaeoecology, Geological Journal, Petroleum Science, Energy Exploration & Exploitation