Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Ian Derry Reid"'
Autor:
Le D. Thang, Henrik I. Petersen, Hans Peter Nytoft, Ioannis Abatzis, Anders Mathiesen, Lars Ole Boldreel, Nguyen Thi Thu Huyen, Ian Derry Reid, Hoang A. Tuan, Dang T. Huong, Nguyen Thi Dau, Lars Henrik Nielsen, L.V. Hien, Michael B.W. Fyhn, Nguyen Anh Duc, Jørgen A. Bojesen-Koefoed
Publikováno v:
Marine and Petroleum Geology. 26:1-24
Seismic stratigraphic and structural analyses of the northwest Phu Khanh Basin, offshore Central Vietnam, based on 2-D seismic data, indicate that the initial rifting began during the latest Cretaceous? or Palaeogene controlled by left-lateral transt
Publikováno v:
Canadian Journal of Earth Sciences. 45:465-481
Data from a refraction seismic profile parallel to the coast of Labrador (Canada) were used to determine the crustal structure across the boundary of the Nain and Makkovik provinces, and to look for evidence for an offshore continuation of the Mesopr
Publikováno v:
Earth and Planetary Science Letters. 182:61-76
There is considerable debate concerning the nature and origin of the thin crust within the ocean^continent transition (OCT) zones of many passive non-volcanic continental margins, located between thinned continental and true oceanic crust. This crust
Autor:
Ian Derry Reid, H. Ruth Jackson
Publikováno v:
Canadian Journal of Earth Sciences. 31:1407-1418
Two densely sampled marine refraction lines were shot in northern Baffin Bay on the shelves of Devon and Ellesmere islands (North American plate) and Greenland (Greenland plate). A total of 11 ocean-bottom seismometers recorded the airgun signals. Th
Publikováno v:
Geology. 23:589
The crust across each margin of the Labrador Sea, a conjugate rift margin pair, consists of three well-defined zones: thinned continental crust, 70–80-km-wide transitional crust, and oceanic crust. The transition zone is characterized by a low-velo
Publikováno v:
Journal of Geophysical Research. 87:1773
Seismic reflection and crustal refraction studies were carried out at the FRAM I ice station near the Arctic Mid-Ocean Ridge crest. This ridge is spreading at the very slow rate of 5 mm yr−1. Upper mantle Pn arrivals with apparent velocities averag