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Basins foreland

DeCelles, P. G. and Hertel, F. (1989). Petrology of fluvial sands from the Amazonian foreland basin. [Pg.225]

United Kingdom Feed coals from 13 fields United Kingdom South Wales Variscan Foreland Basin 26 samples USA Alaska 164 samples... [Pg.184]

Gayer, R.A., Rose, M., Dehmer, J. and Shao, L.-Y. (1999) Impact of sulphur and trace element geochemistry on the utilization of a marine-influenced coal-case study from the South Wales Variscan Foreland Basin. International Journal of Coal Geology, 40(2-3), 151-74. [Pg.209]

DeCelles PG (2004) Late Jurassic to Eocene evolution of the Cordilleran thrust belt and foreland basin system, western U.S.A. Am J Sci 304 105-168... [Pg.17]

Figures 19 and 20 present tentative results that show the application of this approach to the Himalayan foreland basin. Soil carbonate-derived oxygen isotopic compositions from... Figures 19 and 20 present tentative results that show the application of this approach to the Himalayan foreland basin. Soil carbonate-derived oxygen isotopic compositions from...
DeCelles PG, Horton BK (2003) Early to middle Tertiary foreland basin development and the history of Andean crustal shortening in Bolivia. Geol Soc Am Bull 115(l) 58-77 DeCelles PG, Gehrels G, Quade J, Ojha TP (1998) Eocene-early Miocene foreland basin development and the history of Himalayan thrusting, western and central Nepal. Tectonics 17(5) 741-765... [Pg.84]

Hulka C (2005) Sedimentary and tectonic evolution of the Cenozoic Chaco foreland basin, southern Bolivia (Ph. D. dissertation), Freien Universitat, Berlin... [Pg.86]

Talma AS, Netterberg F (1983) Stable isotope abundances in calcretes. In Residual Deposits Surface Related Weathering Processes and Materials. Wilson, RCL (ed) Oxford Blackwell Scientific Publ., p 221-233 Tian L, Masson-Delmotte V, Stievenard M, Tao T, Jouzel J (2001) Tibetan Plateau summer monsoon northward extent revealed by measurements of water stable isotopes. J Geophys Res 106 28,081-28,088 Tian L, Yao T, White JWC, Yu W, Wang N (2005) Westerly moisture transport to the middle of Himalayas revealed from the high deuterium excess. Chinese Sci Bull 50 1026-130 Uba CE, Heubeck C, Hulka C (2006) Evolution of the late Cenozoic Chaco foreland basin, southern Bolivia. Basin Res 18 145-170... [Pg.88]

The volcanic centers of the Campania Province developed inside Quaternary extensional basins along the Tyrrhenian Sea border at the intersection between NE-SW and NW-SE fault systems. The Pontine Islands form a row of volcanoes with a W-E trend, offshore the Campania Province, and along the so-called 41st Parallel Tectonic Line (Serri 1990 Bruno et al. 2000). Vulture is located at the eastern border of the Apennine compression front, in an extensional tectonic setting affecting the border of the Apulia foreland. [Pg.131]

Read J.F. (1980) Carbonate ramp-to-basin transitions and foreland basin evolution, Middle Ordovician, Virginia Appalachians. AAPG Bull. 64, 1575-1612. [Pg.659]

Najman Y., Bickle M., and Chapman H. (2000) Early Himalayan exhumation isotopic constraints from the Indian foreland basin. Terra Nova 12(1), 29-34. [Pg.3423]

Najman Y., Pringle M., Godin L., and Oliver G. (2001) Dating of the oldest continental sediments from the Himalayan foreland basin. Nature 410(6825), 194-197. [Pg.3423]

A. Peripheral (foreland or foredeep) basins (on underriding plate)... [Pg.22]

C. Hinterland foreland, strike-slip, and graben basins (on overriding plate)... [Pg.22]

Figure 2.16 Conceptual model of a foreland basin in a late period of thrusting and uplift (from Ge and Garven, 1989, Geophysical Monograph 48, Fig. 5, p. 148. Copyright by the American Geophysical Union). Figure 2.16 Conceptual model of a foreland basin in a late period of thrusting and uplift (from Ge and Garven, 1989, Geophysical Monograph 48, Fig. 5, p. 148. Copyright by the American Geophysical Union).
Ocean trench foreland basin ( margin) 40 80... [Pg.72]

Hydrodynamic conditions in a basin may in part result from tectonic forces. Ge and Garven (1989) applied a numerical model of coupled tectonic- and gravity-induced flow to evaluate the relative importance of tectonic influence on groundwater pressure and flow in an otherwise gravity-induced flow system in a hypothetical foreland basin. Forbes et al. (1992) included an evaluation of lateral compression in their numerical reconstruction of the present-day pressure distribution in the Venture Field, Eastern Canada. [Pg.243]

See other pages where Basins foreland is mentioned: [Pg.527]    [Pg.527]    [Pg.207]    [Pg.210]    [Pg.211]    [Pg.217]    [Pg.220]    [Pg.287]    [Pg.23]    [Pg.24]    [Pg.46]    [Pg.50]    [Pg.76]    [Pg.103]    [Pg.108]    [Pg.119]    [Pg.144]    [Pg.131]    [Pg.305]    [Pg.305]    [Pg.1463]    [Pg.2648]    [Pg.3599]    [Pg.3606]    [Pg.3621]    [Pg.3838]    [Pg.22]    [Pg.52]    [Pg.53]    [Pg.53]    [Pg.66]    [Pg.75]    [Pg.77]    [Pg.78]   
See also in sourсe #XX -- [ Pg.52 , Pg.53 , Pg.75 , Pg.77 , Pg.78 , Pg.243 ]



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Foreland basins, northern Apennines

North Alpine Foreland Basin

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