Zobrazeno 1 - 10
of 28
pro vyhledávání: '"J. F Dewey"'
Autor:
J. F. Dewey, R. Graham
Publikováno v:
Biographical Memoirs of Fellows of the Royal Society. 74:363-385
John Ramsay was a scientific polymath, the finest structural geologist of his generation, with superb field mapping skills and a solid grasp of mathematics and engineering. He was also accomplished as a cellist, painter in oils, runner, cyclist, ling
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c71db25479eaafc9b95307bd752b8b1b
https://doi.org/10.1098/rsbm.2022.0031
https://doi.org/10.1098/rsbm.2022.0031
Publikováno v:
Natural Hazards. 109:1981-2002
We identify 14 mechanisms, marine and non-marine, one man made, that result and could result in the formation of boulder deposits after reviewing issues associated with clast shape, size and classification. Four of these mechanisms: storm deposits; w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a2fb81767812869b59ef374130024c8
https://doi.org/10.1007/s11069-021-04906-3
https://doi.org/10.1007/s11069-021-04906-3
Autor:
J. F. Dewey, P. N. Taylor
Stephen Moorbath was an intellectual with eclectic interests across the sciences and humanities. In 1939, as a ten-year-old, he fled from Germany to England with his father. Stephen spent almost the whole of the rest of his life—from schoolboy to u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::30e904612d5361fb34cd3224e3cb104f
Publikováno v:
Geological Society, London, Special Publications. 335:383-404
The Moine Thrust zone ofNWScotland marks the Caledonian orogenic front and in the Assynt region consists of several west-vergent major thrust sheets (Moine, Ben More, Glencoul and Sole Thrust sheets) that place allochthonous rocks onto the Lewisian b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2731c1617637e7d271e775f2fe342908
https://doi.org/10.1144/sp335.18
https://doi.org/10.1144/sp335.18
Autor:
J. F. Dewey
Publikováno v:
Geological Journal. 6:193-216
Although the deformation of foliated rocks by kink and glide mechanisms has been studied in detail in recent years, fundamental differences of opinion have emerged, particularly as a result of experimental work. Most theories concerning the relations
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e467d790f47277b3dc4d5143b9093a23
https://doi.org/10.1002/gj.3350060206
https://doi.org/10.1002/gj.3350060206
Autor:
W. E. A. Phillips, J. F. Dewey
Publikováno v:
Geological Journal. 3:237-246
A composite tectonic profile, from Clew Bay to central Murrisk is constructed and the sequence of structural events from the Upper Cambrian to post-Wenlock—pre-Visean (C2 S2) times is outlined. Four main structural episodes affected the Dalradian r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::58386b2c5034c3ad8320c6f6c2962540
https://doi.org/10.1002/gj.3350030202
https://doi.org/10.1002/gj.3350030202
Autor:
J. F. Dewey
Publikováno v:
Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. 331:643-647
During the course of this Discussion Meeting, a very large amount of regional tectonic geology was displayed, and debated critically in a terrane framework, on scales ranging from the whole of the North American Precambrian or the Mesozoic-Cenozoic T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::00821de122d2670abb8e4713b0ddfa97
https://doi.org/10.1098/rsta.1990.0096
https://doi.org/10.1098/rsta.1990.0096
Autor:
J. F. Dewey
Publikováno v:
Mineralogical Magazine. 65:462-462
The principal theme of this book is the idea that many features of plate boundaries and plate motion are the direct result of major bolide impacts throughout the Earth’s history. The book is in four parts. First, there is a detailed outline of plat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d37e73190a22f0dabd5f59e41b698ba
https://doi.org/10.1180/s0026461x00029935
https://doi.org/10.1180/s0026461x00029935
Publikováno v:
Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. 331:641-641
A. Trench (Department of Earth Sciences, University of Oxford, U. K. ). Several participants at the meeting commented upon the impact of the terrane hypothesis in directing geological thinking to consider strike-slip movements within the British Cale
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::770cdbb562ca217bd76db509335007bf
https://doi.org/10.1098/rsta.1990.0095
https://doi.org/10.1098/rsta.1990.0095
Publikováno v:
Journal of the Geological Society. 136:303-310
The age difference of oceanic crust on opposite sides of a fracture zone results in a depth differential and in different subsidence rates on the two sides. There is thus a component of dip-slip motion along the entire length of a fracture zone that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b2432c7686784036c5d7609756ebf925
https://doi.org/10.1144/gsjgs.136.3.0303
https://doi.org/10.1144/gsjgs.136.3.0303