Moho topography beneath the Iberian-Western Mediterranean region mapped from controlled-source and natural seismicity surveys, Tectonophysics 692, 74-95.Diaz, J., Gallart, J., & Carbonell, R. (2016). Moho topography beneath the Iberian-western Mediterranean region mapped from controlled- source and...
It is the purpose of this review to tease out and map a Palaeozoic history for the region (Fig. 1) and to consider its changing palaeogeography through time. One practical problem is the deluge of data that has accumulated from North America and its marginal areas over the past two ...
Western Patagonia is a vast (~400,000 km2), narrow (~200–300 km) and transboundary (Chile and Argentina) area extending from about 40°S down to the southern tip of the continent (40–56°S; Fig.1). It is one of the largest and best preserved freshwater ecosystems in the world...
including the areas studied in this paper); Pi (Pyrenees), Pb (Prebetics of the External Betic Zone), Ri (Ghomarides and Dorsal of the Internal Rifian Zone), Mo (Moroccan External Zone), Tu (Tunisian Tell); C) Synthetic geological map of the Betic Cordillera with location of the stud...
Application of remote sensing technologies to map the structural geology of Central Region of Kenya. IEEE J. -Stars 8, 1855–1867 (2015). Google Scholar Song, C. Q., Huang, B. & Ke, L. H. Heterogeneous change patterns of water level for inland lakes in High Mountain Asia derived ...
Despite the evidence for protracted deformation, crustal shortening, and exhumation since at least 100 Ma along the Central Andes, the uplift of the Eastern Cordillera and Bolivian Orocline formation did not start until the Eocene–Oligocene. Moreover, the Central Andes also exhibit much younger ...
Geochemistry of Cretaceous to Eocene ophiolitic rocks of the Central Cordillera: implications on the Mesozoic-early Cenozoic evolution of northern Philippines Int. Geol. Rev., 50 (2008), pp. 407-421 CrossrefView in ScopusGoogle Scholar Queaño et al., 2013 K.L. Queaño, E.J. Marquez, ...
• Sequence stratigraphic and depositional models of the Porto Torres Basin are revised. • The climatic control is increasing at the transition from the syn-to postrift stage. • Rhodalgal slope progradation in Sardinia at the onset of the postrift stage. ...
(a–e). The shaded region in blue, red and white represents cluster-1, cluster-2 and missing dates. Spatial map (f) of HYSPLIT clustered backward trajectories at Mahabaleshwar receptor site (MBLR), mapped over ASCAT ocean surface wind stress (Pa). And local AWS clustered wind rose diagram...
A symposium on the Progress of Gravity Surveys in the western United States was held at the University of Colorado, Boulder, on December 27 and 28, 1963, as part of the Western National Meeting of the AGU. The object of the symposium was to provide an up to date picture of surveys comp...