| Orbitally-paced climate change in the early Cambrian and its implications for the history of the Solar System T Zhang, Y Li, T Fan, AC Da Silva, J Shi, Q Gao, M Kuang, W Liu, Z Gao, ... Earth and Planetary Science Letters 583, 117420, 2022 | 49 | 2022 |
| Laminar characteristics of lacustrine organic-rich shales and their significance for shale reservoir formation: A case study of the Paleogene shales in the Dongying Sag, Bohai … J Shi, Z Jin, Q Liu, T Zhang, T Fan, Z Gao Journal of Asian Earth Sciences 223, 104976, 2022 | 31 | 2022 |
| Cyclostratigraphy of Lower Triassic terrestrial successions in the Junggar Basin, northwestern China T Zhang, C Zhang, T Fan, L Zhang, R Zhu, J Tao, M Li Palaeogeography, Palaeoclimatology, Palaeoecology 539, 109493, 2020 | 19 | 2020 |
| Marine carbon and sulfur cycling across the Ediacaran-Cambrian boundary in Tarim Block and its implications for paleoenvironmental changes T Zhang, Y Li, T Fan, G Lash, Z Gao, Q Fan Palaeogeography, Palaeoclimatology, Palaeoecology 560, 110011, 2020 | 16 | 2020 |
| Geochemistry of the Lower Silurian black shales from the Upper Yangtze Platform, South China: Implications for paleoclimate, provenance, and tectonic setting M Ding, Y Li, T Fan, G Lash, X Wei, T Zhang Journal of Asian Earth Sciences 242, 105493, 2023 | 10 | 2023 |
| Orbitally-paced climate change during the Carnian Pluvial Episode Q Zhang, X Fu, J Wang, A Mansour, H Wei, T Zhang, M Wang Earth and Planetary Science Letters 626, 118546, 2024 | 7 | 2024 |
| Astronomical Forcing of Sea‐Level Changes and the History of the Solar System 1,640 Million Years Ago J Shi, T Fan, Z Jin, Q Liu, T Zhang, M Jiang, B Wang Journal of Geophysical Research: Solid Earth 128 (10), e2023JB027050, 2023 | 7 | 2023 |
| 准噶尔盆地玛湖凹陷百口泉组相对湖平面升降规律研究 张坦， 张昌民， 瞿建华， 朱锐， 袁瑞， 潘进， 陶金雨 沉积学报 36 (4), 684-694, 2018 | 7 | 2018 |
| Orbital forcing of tropical climate dynamics in the Early Cambrian T Zhang, Y Li, T Fan, AC Da Silva, M Kuang, W Liu, C Ma, Q Gao, J Shi, ... Global and Planetary Change 219, 103985, 2022 | 6 | 2022 |