Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Anekant M Wandres"'
Publikováno v:
New Zealand Journal of Geology and Geophysics. 48:229-245
The Torlesse terranes—part of the New Zealand Eastern Province—are accretionary complexes that comprise an enormous volume of quartzofeldspathic sandstones and mudstones with subsidiary conglomerates plus minor oceanic assemblages. Two terranes a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c7af56c4183d2b734d7fa634121a8598
https://doi.org/10.1080/00288306.2005.9515112
https://doi.org/10.1080/00288306.2005.9515112
Autor:
Anekant M Wandres, John D. Bradshaw
Publikováno v:
Geological Society, London, Special Publications. 246:179-216
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b6a5dca3b3b3532e5ff7024d340f54a9
https://doi.org/10.1144/gsl.sp.2005.246.01.06
https://doi.org/10.1144/gsl.sp.2005.246.01.06
Publikováno v:
Sedimentary Geology. 168:193-226
The Permian to Late Triassic Rakaia sub-terrane—part of the Torlesse superterrane of the New Zealand Eastern Province—is an accretionary complex that comprises an enormous volume of quartzofeldspathic sandstones and mudstones with subsidiary cong
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a68a53f9e7ac52908950aa2a96caa88
https://doi.org/10.1016/j.sedgeo.2004.03.003
https://doi.org/10.1016/j.sedgeo.2004.03.003
Publikováno v:
Sedimentary Geology. 167:57-89
The field of provenance analysis has undergone a revolution with the development of single-crystal isotope dating techniques using mainly silt to sand sized single minerals. This study focuses on coarser-grained rocks, notably conglomerates, which in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f8693e8517fc331260ec74dccfb1431c
https://doi.org/10.1016/j.sedgeo.2004.02.002
https://doi.org/10.1016/j.sedgeo.2004.02.002
Publikováno v:
New Zealand Journal of Geology and Geophysics. 41:1-14
The Early Cretaceous Darran Complex of the Median Tectonic Zone near Milford, South Island, New Zealand, consists dominantly of biotite ‐ two‐pyroxene diorites cut by biotite‐hornblende microdiorite and quartz monzodiorite dikes. The host diori
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d8d53981acc14cbbb6fabba5a867894d
https://doi.org/10.1080/00288306.1998.9514786
https://doi.org/10.1080/00288306.1998.9514786