Zobrazeno 1 - 10
of 87
pro vyhledávání: '"Peter Copeland"'
Autor:
Suoya Fan, Michael A. Murphy, David M. Whipp, Joel E. Saylor, Peter Copeland, Andrew K. Hoxey, Michael H. Taylor, Daniel F. Stockli
Between 81 degrees 30MODIFIER LETTER PRIMEE and 83 degrees E, the Himalayan range's "perfect" arcuate shape is interrupted by an embayment. We hypothesize that thrust geometry and duplexing along the megathrust at midlower-crustal depths play a leadi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::99d8a6acd70882ae3791e753fef0759f
https://doi.org/10.1002/essoar.10507987.2
https://doi.org/10.1002/essoar.10507987.2
Autor:
Shelby, Johnston, Alan, Brandon, Claire, McLeod, Kai, Rankenburg, Harry, Becker, Peter, Copeland
Publikováno v:
Nature. 611(7936)
Reconstructing the building blocks that made Earth and the Moon is critical to constrain their formation and compositional evolution to the present. Neodymium (Nd) isotopes identify these building blocks by fingerprinting nucleosynthetic components.
Autor:
Claire A. Currie, Peter Copeland
Publikováno v:
Geosphere.
Flat-slab subduction has affected parts of North America, South America, and Asia over the past 250 m.y. In these areas, reconstructions show that the subducting plate became subhorizontal below the continent for ~5 to >30 m.y., followed by founderin
Autor:
Peter Copeland, Claire A. Currie
Animations 1, 2, and 3. Animation 1. Evolution of Model 1 showing the full model domain. Animation 2. Evolution of Model 9 showing the full model domain. Animation 3. Evolution of Model 23 showing the full model domain.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3871b22d400c5fe70281d00d80801775
https://doi.org/10.1130/geos.s.16920472.v3
https://doi.org/10.1130/geos.s.16920472.v3
Autor:
Peter Copeland
Publikováno v:
Basin Research. 32:1532-1546
[Clastic sedimentary rocks are best dated by isotopic analysis of closely interbedded volcanic rocks (PLAN A). Fossils can also provide age assement of sufficient precision (PLAN B) but when volcanic rocks are not present or fossils are not diagnosti
Autor:
Peter Copeland, Claire A. Currie
Animations 1, 2, and 3.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0899f471ab40ff67608719a936d47892
https://doi.org/10.1130/geos.s.16920466.v1
https://doi.org/10.1130/geos.s.16920466.v1
Autor:
Peter Copeland, Daniel F. Stockli, Andrew K.R. Hoxey, Suoya Fan, Michael A. Murphy, David Whipp, Michael H. Taylor, Joel E. Saylor
Between 81o30’ E and 83oE the Himalayan range’s “perfect” arcuate shape is interrupted by an embayment. We hypothesize that thrust geometry and duplexing along the megathrust at mid-lower...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a2ad74894186a583b6ae48ec3585d06
https://doi.org/10.1002/essoar.10507987.1
https://doi.org/10.1002/essoar.10507987.1
Autor:
Peter Copeland, Luigi Solari, Ashley Ngyuen, Timothy F. Lawton, Jarret Garber, Marie G. De los Santos, Sarah Dailey, Shantel White, Viktor Herrera, Callum Byers, Stuart A. Hall
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Tectonics. 39