Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Thomas N. Lamont"'
Autor:
Thomas N. Lamont, Nick M.W. Roberts, Michael P. Searle, Nicholas J. Gardiner, Phillip Gopon, Yu-Te Hsieh, Philip Holdship, Richard W. White
Publikováno v:
GSA Bulletin.
Granitoids of varying mineralogy are exposed on the Cycladic islands of Greece; they include both hornblende-bearing I-type granites and garnet ± muscovite−bearing S-type granites, suggesting heterogeneous magma sources. In this contribution, we p
Autor:
Thomas N. Lamont, Andrew J. Smye, Nick M.W. Roberts, Michael P. Searle, David J. Waters, Richard W. White
Publikováno v:
GSA Bulletin.
Metamorphic core complexes are classically interpreted to have formed during crustal extension, although many also occur in compressional environments. New U−(Th)−Pb allanite and xenotime geochronologic data from the structurally highest Zas Unit
Autor:
Thomas N. Lamont
Further method details and complete results for granite geochemistry, Sr-Nd isotope analysis, and U-Pb geochronology.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3149e8f4363503698594f5e3d2d5ef0f
https://doi.org/10.1130/gsab.s.21325902.v1
https://doi.org/10.1130/gsab.s.21325902.v1
Autor:
Thomas N. Lamont
Further method details of U–(Th)–Pb geochronology and thermal modelling and complete U–(Th)–Pb analyses.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8c8cbe29d67447d7422c715da21539a4
https://doi.org/10.1130/gsab.s.21266472.v1
https://doi.org/10.1130/gsab.s.21266472.v1
Autor:
Andrew J. Smye, Thomas N. Lamont, Michael P. Searle, O. M. Weller, David J. Waters, Phillip Gopon, Marc R. St-Onge, Nick M.W. Roberts, Brendan Dyck, Richard M. Palin
Publikováno v:
GSA Bulletin. 132:149-197
The island of Naxos, Greece, has been previously considered to represent a Cordilleran-style metamorphic core complex that formed during Cenozoic extension of the Aegean Sea. Although lithospheric extension has undoubtedly occurred in the region sinc
Autor:
Michael P. Searle, Thomas N. Lamont
Publikováno v:
Geological Magazine. 157:101-118
Metamorphic core complexes (MCCs) are interpreted as domal structures exposing ductile deformed high-grade metamorphic rocks in the core underlying a ductile-to-brittle high-strain detachment that experienced tens of kilometres of normal sense displa
Autor:
Kyaw Min Htun, David J. Waters, Bradley R. Hacker, Christopher K. Morley, Michael P. Searle, Kyi Htun, Thomas N. Lamont, Richard White
MPS is grateful to the Oxford-Burma Aung San Suu Kyi trust for funding research and field visits to Mogok. U-Th-Pb geochronology was funded by UCSB and NSF grants EAR-1348003 and EAR-1551054 to BH. The Mogok Metamorphic Belt (MMB) in Myanmar is a pol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9300efa41af5b995925b6283d7fa8f1d
https://hdl.handle.net/10023/24809
https://hdl.handle.net/10023/24809
Autor:
Thomas N. Lamont, Michael P. Searle
Publikováno v:
Geoscience Frontiers. 13:101049
The Aegean Sea area is thought to be an actively extending back-arc region, north of the present day Hellenic volcanic arc and north-dipping subduction zone in the Eastern Mediterranean. The area shows extensive normal faulting, ductile ‘extensiona
Autor:
Richard M. Palin, Thomas N. Lamont, Michael P. Searle, Phillip Gopon, David J. Waters, Jon Wade, Nick M.W. Roberts
Publikováno v:
Tectonics. 39
This work forms part of T. N. Lamont’s doctoral project which is funded by the Natural Environment Research Council (Grant No. NE/L0021612/1) and the University of Oxford for covering publication fees. High pressure–low temperature (HP–LT ) met
Autor:
Jon Wade, David J. Waters, Nick M.W. Roberts, Michael P. Searle, Phillip Gopon, Thomas N. Lamont, Richard White
The Attic-Cycladic Massif (ACM) preserves the entire evolution of a NE dipping subduction zone. This includes the intra-oceanic subduction initiation associated with ophiolite obduction and formation of a metamorphic sole, to subduction-termination a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e04bea74994b4caa79e8f3ea1f6c7de
https://doi.org/10.5194/egusphere-egu2020-21985
https://doi.org/10.5194/egusphere-egu2020-21985