Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Lewis H. King"'
Autor:
Lewis H. King
Publikováno v:
Geological Society of America Bulletin. 108:1056-1067
The late middle to late Wisconsinan Laurentide ice sheet terminated at the edge of the Scotian Shelf ca. 21 ka, in close temporal agreement with the H-2 Heinrich event of the North Atlantic stratigraphy. The ice began its recession along the western
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df03a8d70f633ab0672c75540861435c
https://doi.org/10.1130/0016-7606(1996)108<1056:lwirft>2.3.co
https://doi.org/10.1130/0016-7606(1996)108<1056:lwirft>2.3.co
Autor:
Lewis H. King
Publikováno v:
Canadian Journal of Earth Sciences. 31:401-417
A refined synthesis of the stratigraphy of the Scotian Shelf is presented, based on recently published borehole and seismic-reflection data and detailed correlation along high-resolution seismic profiles between the outer banks and the central basins
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eaf588e611ae3c3541dfe953cbb71901
https://doi.org/10.1139/e94-037
https://doi.org/10.1139/e94-037
Autor:
Lewis H. King
Publikováno v:
Journal of Quaternary Science. 8:347-358
Till is of common occurrence in the marine environment and can be both subglacial and proglacial in origin. Former glacial margins are often represented by till tongues, that are interbedded with stratified glaciomarine sediment, and the relationship
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c04b8691e5bff4f61371a3ce2a551e1
https://doi.org/10.1002/jqs.3390080406
https://doi.org/10.1002/jqs.3390080406
Publikováno v:
Geological Society of America Bulletin. 103:637-659
Seismostratigraphic studies on the Scotian and mid-Norwegian Continental Shelves have led to the development of a conceptual model for glacial deposition and erosion by ice sheets in a marine environment (till-tongue model). Some of the terminal depo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e54421b1760ba1fd397966e76e3d6a04
https://doi.org/10.1130/0016-7606(1991)103<0637:tts>2.3.co
https://doi.org/10.1130/0016-7606(1991)103<0637:tts>2.3.co
Publikováno v:
Canadian Journal of Earth Sciences. 23:504-526
Analyses of seismic reflection profiles supported by lithological and palynological studies of core samples from submarine outcrops indicate that the lower Paleozoic succession of the Avalon Terrane, southeast Newfoundland, is continuous offshore. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e7b1e056d09415aabcea94d4c7c478ba
https://doi.org/10.1139/e86-052
https://doi.org/10.1139/e86-052
Publikováno v:
Canadian Journal of Earth Sciences. 11:89-100
Four erosional unconformities have been recognized within the Mesozoic-Cenozoic succession on the Scotian Shelf, on the basis of data from high resolution seismic reflection profiles. Older unconformities are known from well data and others may be re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55c47ca7fd7f670485b60bd8388c9808
https://doi.org/10.1139/e74-008
https://doi.org/10.1139/e74-008
Publikováno v:
Sedimentology. 31:471-480
This paper presents the results of a comparative study of pockmarks and associated features appearing on both sides of the North Atlantic: on the Scotian Shelf off Nova Scotia and in the northern North Sea. Pockmarks are formed in seabed material con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::23339dd9c5eb110bc384b281b2ec0a80
https://doi.org/10.1111/j.1365-3091.1984.tb01813.x
https://doi.org/10.1111/j.1365-3091.1984.tb01813.x
Autor:
Ian F. Young, Lewis H. King
Publikováno v:
Canadian Journal of Earth Sciences. 14:2553-2564
A study of processed seismic reflection profiles along the eastern Canadian continental margin indicates the occurrence at depth of paleocontinental slopes of Cenozoic–Mesozoic age, generally in the vicinity of the present continental slope. The pa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4bf66790ffb7ec301743179d55d17309
https://doi.org/10.1139/e77-221
https://doi.org/10.1139/e77-221
Publikováno v:
Canadian Journal of Earth Sciences. 15:831-840
Pockmarks, cone-shaped depressions that occur in unconsolidated fine sediments at the seabed, are generally thought to be formed by gas ascending from underlying sediments. A mosaic of pockmarks in Emerald Basin on the Scotian Shelf was constructed a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f88cc15d676b3bd0ba4a475ead6087f8
https://doi.org/10.1139/e78-088
https://doi.org/10.1139/e78-088
Autor:
Lewis H. King
Publikováno v:
Canadian Journal of Earth Sciences. 13:1082-1092
A side-scan sonar survey along the western bank of the Laurentian Channel and on the western Grand Banks revealed the occurrence of iceberg furrows that are probably of Late Pleistocene age. The occurrence of furrows in the Gulf of St. Lawrence is si
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f098b0a6098596be2214cfe5292ab11b
https://doi.org/10.1139/e76-111
https://doi.org/10.1139/e76-111