Items/Page: Sort: |
| Response of Yunnan crustal structure to eastward growth of the Tibet Plateau and subduction of the India plate in Cenozoic [期刊论文] Tectonophysics, 2020-01-01, 797 Ling Y.; Zheng T.; He Y.; Hou G.
View/Download:2/0 |
| Late Miocene accelerated exhumation in the central Tajik Basin and implications for northward indention and lateral growth of the Pamir [期刊论文] Tectonophysics, 2020-01-01, 787 Lü L.; Sun J.; Zhang Z.; Jia Y.; Tian S.; Abdulov S.; Gadoev M.; Oimahmadov I.
View/Download:6/0 |
| Jurassic intracontinental deformation of the central North China Plate: Insights from syn-tectonic sedimentation, structural geology, and U[sbnd]Pb geochronology of the Yungang Basin, North China [期刊论文] Tectonophysics, 2020-01-01, 778 Zhang Y.; Shi W.; Dong S.; Wang T.; Yang Q.
View/Download:3/0 |
| Estimating the formation age distribution of continental crust by unmixing zircon ages [期刊论文] Earth and Planetary Science Letters, 2018-01-01, 482 Korenaga J.
View/Download:11/0 |
| A new hypothesis for the initiation of plate tectonics on Earth: Feedback between subduction and continental crust growth [项目] Bradford Foley
View/Download:15/0 |
| Cretaceous Vertebrates from Madagascar: A Window into the Biogeographic and Plate Tectonic History of Gondwana [项目] David Krause
View/Download:21/0 |
| Collaborative Research: Cretaceous Vertebrates from Madagascar: A Window into the Biogeographic and Plate Tectonic History of Gondwana [项目] Patrick O'; Connor
View/Download:20/0 |
| Cretaceous Vertebrates from Madagascar: A Window into the Biogeographic and Plate Tectonic History of Gondwana [项目] David Krause
View/Download:22/0 |
| BRIGE: Delivery of Silencing RNA and TGF-b1 from Biopolymer Hydrogels to Inhibit Osteogenesis and Promote Chondrogenesis in Growth Plate Injuries [项目] Melissa Krebs
View/Download:8/0 |
| Timescales of Development of Sub-Ophiolite Subduction: High Precision U-Pb Dating and Geochemical Characterization of Late Magmatism and Metamorphism in the Oman-U.A.E. Ophiolite [项目] Matthew Rioux
View/Download:2/0 |