Zobrazeno 1 - 10
of 25
pro vyhledávání: '"Douglas W. Rankin"'
Autor:
Sheila J. Seaman, Aránzazu Piñán-Llamas, M. Chapman, Douglas W. Rankin, R. Hon, Reinhard A. Wobus, G.C. Koteas, J.P. Hogan, J.C. Hepburn, M. Whitman
Publikováno v:
GSA Bulletin. 131:1995-2010
Contemporaneous mafic and felsic magmatism occurs in a variety of tectonic settings where continental crust is invaded by mantle-derived basaltic melt. Bimodal magmatism, including supervolcano-scale eruptions, occurred in both the Coastal Maine magm
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9866a77b738c1ef81973591453105393
https://doi.org/10.1130/b32058.1
https://doi.org/10.1130/b32058.1
Autor:
Douglas W. Rankin
Publikováno v:
Open-File Report.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9822b280f19194574d09120bf4006aa8
https://doi.org/10.3133/ofr20181025
https://doi.org/10.3133/ofr20181025
Autor:
Douglas W. Rankin
Publikováno v:
Open-File Report.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f830d67c3e6b959f9b922dfee68852db
https://doi.org/10.3133/ofr20181087
https://doi.org/10.3133/ofr20181087
Autor:
Douglas W. Rankin
Publikováno v:
Open-File Report.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::810af017d68f40af5d2935e94803e08a
https://doi.org/10.3133/ofr20181016
https://doi.org/10.3133/ofr20181016
Publikováno v:
Geological Society of America Bulletin. 125:998-1024
The regional extent and mode and time of emplacement of the Piermont-Frontenac allochthon in the Boundary Mountains–Bronson Hill anticlinorium of the Upper Connecticut Valley, New Hampshire–Vermont, are controversial. Moench and coworkers beginni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e4c56faa129705bc53de7bfcfc6e3e1
https://doi.org/10.1130/b30590.1
https://doi.org/10.1130/b30590.1
Autor:
Leon T. Silver, Robert S. Houston, Douglas W. Rankin, Mitchell W. Reynolds, P. K. Sims, John C. Reed
Precambrian rocks are at or near the surface in only about 10 percent of the conterminous United States, but it can reasonably be inferred that they comprise the continetal crust beneath about 90 percent. They are missing or unrecognized in the exoti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b01cbc09708fa7586bab46146110e853
https://doi.org/10.1130/dnag-spec-v1.7
https://doi.org/10.1130/dnag-spec-v1.7
Publikováno v:
Precambrian Research. 128:3-38
Emplacement of compositionally distinctive granitic plutons accompanied two pulses (765–680 and 620–550 Ma) of crustal extension that affected the Rodinian craton at the present location of the central Appalachians during the Neoproterozoic. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dc427f3d89d52caae7b55ea36dae199a
https://doi.org/10.1016/j.precamres.2003.08.007
https://doi.org/10.1016/j.precamres.2003.08.007
Autor:
Douglas W. Rankin, Mary B. Rankin
Publikováno v:
Open-File Report.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::934906c81f0b28c82185ef23427130c7
https://doi.org/10.3133/ofr20141026
https://doi.org/10.3133/ofr20141026