Zobrazeno 1 - 10
of 141
pro vyhledávání: '"Tim E. Johnson"'
Autor:
Bo Huang, Man Liu, Timothy M. Kusky, Tim E. Johnson, Simon A. Wilde, Dong Fu, Hao Deng, Qunye Qian
Publikováno v:
Nature Communications, Vol 14, Iss 1, Pp 1-14 (2023)
Abstract The Earth’s interior and surficial systems underwent dramatic changes during the Paleoproterozoic, but the interaction between them remains poorly understood. Rocks deposited in orogenic foreland basins retain a record of the near surface
Externí odkaz:
https://doaj.org/article/68976663793646629fb5a44a182ad736
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-13 (2022)
This study reports coexisting Neoarchean divergent and convergent plate boundary rock assemblages, providing new evidence for the operation of plate tectonics 2.55–2.51 billion years ago; and also suggests the subduction zone was warm then.
Externí odkaz:
https://doaj.org/article/756af53ffaa24b709fa5f7346f4e6dc0
Autor:
Robert H. Smithies, Yongjun Lu, Tim E. Johnson, Christopher L. Kirkland, Kevin F. Cassidy, David C. Champion, David R. Mole, Ivan Zibra, Klaus Gessner, Jyotindra Sapkota, Matthew C. De Paoli, Marc Poujol
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-12 (2019)
Some of Earth’s earliest continental crust has been previously inferred to have formed from partial melting of hydrated mafic crust at pressures above 1.5 GPa (more than 50 km deep), pressures typically not reached in post-Archean continental crust
Externí odkaz:
https://doaj.org/article/7ec8b46796a14bc88ba5c9941ac2f6c4
Autor:
Tim E. Johnson, Christopher L. Kirkland, Yongjun Lu, R. Hugh Smithies, Michael Brown, Michael I. H. Hartnady
Publikováno v:
Nature. 608:330-335
Publikováno v:
Journal of Petrology. 64
The bulk rock composition of granitoids reflects the composition of their source and the conditions of partial melting, which are functions of the geodynamic setting in which they formed. Granitoids in active continental margins (continental arcs) ar
Autor:
Songjie Wang, Michael Brown, Lu Wang, Tim E. Johnson, Hugo K.H. Olierook, Christopher L. Kirkland, Andrew Kylander-Clark, Noreen J. Evans, Bradley J. McDonald
Publikováno v:
GSA Bulletin. 135:48-66
The rates and mechanisms by which deeply subducted continental crust was exhumed back to the surface are not well understood, but can be better characterized using multimineral petrochronology. Here, we combine zircon, titanite, and apatite U-Pb ages
Publikováno v:
Geology. 50:631-635
Since the Jurassic, there has been a clear spatiotemporal correlation between different types of metamorphism and active convergent plate margins. However, the extent to which this relationship extends into the past is poorly understood. We compared
Autor:
Tim E. Johnson, Ali Polat, Fred Jourdan, Timothy M. Kusky, Bo Huang, Zhaochu Hu, Dong Fu, Simon A. Wilde, Brian F. Windley
Publikováno v:
Geology. 50:10-15
Subduction of oceanic lithosphere is a diagnostic characteristic of plate tectonics. However, the geodynamic processes from initiation to termination of subduction zones remain enigmatic mainly due to the scarcity of appropriate rock records. We repo
Publikováno v:
South African Journal of Geology. 124:37-52
The continental crust that dominates Earth’s oldest cratons comprises Eoarchaean to Palaeoarchaean (4.0 to 3.2 Ga) felsic intrusive rocks of the tonalite-trondhjemite-granodiorite (TTG) series. These are found either within high-grade gneiss terran
Publikováno v:
Acta Geologica Sinica - English Edition. 95:65-67