Zobrazeno 1 - 10
of 25
pro vyhledávání: '"Roy Kligfield"'
Publikováno v:
Unconventional Resources Technology Conference, Denver, Colorado, 12-14 August 2013.
Publikováno v:
Tectonophysics. 225:231-254
Measurements of finite strain, the anisotropy of magnetic susceptibility, the magnetic carrier of the susceptibility, and fieldwork have been carried out in the Onaping Formation of the Sudbury Basin, Ontario. The magnetic fabric indicates that chang
Autor:
Luigi Carmignani, Roy Kligfield
Publikováno v:
Tectonics. 9:1275-1303
An interpretation of Northern Apennine geology is presented which relates the temporal and spatial occurrence of both compressional and extensional deformation features in terms of the changing dynamic evolution within an accretionary wedge, after a
Autor:
Antonio Lazzarotto, Marco Meccheri, F. A. Decandia, D. Liotta, Pier Lorenzo Fantozzi, Leonardo Disperati, Roy Kligfield, Luigi Carmignani
Publikováno v:
Anatomy of an Orogen: the Apennines and Adjacent Mediterranean Basins ISBN: 9789048140206
The Northern Apennines are a fold—thrust belt formed during the Tertiary by the tectonic superposition from W to E of the Ligurides on the Tuscan nappe and on the Tuscan metamorphic complex (Boccaletti et al., 1971; Alvarez et al., 1974; Kligfield,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::67bf5e5f607775667c5b5e846fd1b050
https://doi.org/10.1007/978-94-015-9829-3_14
https://doi.org/10.1007/978-94-015-9829-3_14
Publikováno v:
AAPG Bulletin. 82
Exploration and development activity has increased significantly during the past 5 years in the northern deep Gulf of Mexico. This activity has been caused by several factors, including significant discoveries in deep water (>1500-ft water depth), ou
Autor:
Roy Kligfield, Mark G. Rowan
Publikováno v:
Thrust Tectonics ISBN: 9780412439001
Kinematic analysis of asymmetric detachment folds from the Wildhorn nappe, central Helvetics, Switzerland, supports models of buckle fold formation in overthrust shear between nappe boundaries. The overall geometry shows a 2500 m thick multilayer of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::87b7dd52ae1cca685b811ee5ab201d4e
https://doi.org/10.1007/978-94-011-3066-0_14
https://doi.org/10.1007/978-94-011-3066-0_14
Publikováno v:
Geology. 19:1001
Volume loss due to pressure solution along spaced cleavage and volume gain represented by dilatant veins have been quantified for folded carbonates from the Helvetic nappes. Samples from two formations with low clay contents (
Publikováno v:
Tectonophysics. 145:191-211
Cleavage formation in the Precambrian Chelmsford Formation of the Sudbury Basin, Ontario, is directly related to the finite strain and deformation path. Finite strain was measured at the outcrop scale from the shapes and orientations of deformed conc