Titlebook: New Perspectives in Basin Analysis; Karen L. Kleinspehn,Chris Paola Book 1988 Springer-Verlag New York Inc. 1988 Chronostratigraphy.Erosio

thrombus

Provenance and Sediment Dispersal in Relation to Paleotectonics and Paleogeography of Sedimentary Baedict reliably the nature of the petrofacies that some basins contain. Adequate evaluation of sedimentary linkages between varied provenances and basins requires improved understanding of regional paleo-geomorphology and an integrated view of global sediment dispersal..Sediment dispersal is controll

Delude

喧鬧

History of Uplift and Relief of the Himalaya During the Past 18 Million Years: Evidence from Fissionyears. These ages imply that a series of uplifted blocks or “massifs,” analogous to the contemporary Nanga Parbat area, have been continually present in the Himalaya since 18 Ma, and that over that time the elevation and relief of the Himalaya, on a broad scale, have been essentially constant.

噴油井

Facies Architecture in Clastic Sedimentary Basinsral elements.” The lithofacies composition, external shape, and internal geometry of these elements are characteristic of various suites of processes in depositional systems; for example, the well known lateral-accretion deposit represents the accretion of bank-attached bars inside meander bends of

暗諷

Origin, Recognition, and Importance of Erosional Unconformities in Sedimentary Basinsnition of unconformities is useful for subdividing stratigraphic units, determining the timing of tectonic activity, interpreting lateral facies relationships, constructing burial and uplift curves, correlating certain stratigraphic boundaries, interpreting sea-level changes, and for reconstructing

intuition

Analysis of Eustatic, Tectonic, and Sedimentologic Influences on Transgressive and Regressive Cyclesuch of the section to a Pleistocene sea-level curve determined from oxygen-isotope data. If eustatic fluctuations can be subtracted from the stratigraphic record, tectonic and sedimentologic influences become evident. The accumulation of such a thick succession of shallow-marine and coastal deposits

大暴雨

Cambro-Ordovician Eustasy: Evidence from Geophysical Modelling of Subsidence in Cordilleran and Appasingle, long-term rise and fall spanning more than 40 million years and the other consisting of multiple, short-term changes, lasting from 2 to 10 million years, that are superimposed on the long-term event. The long-term event coincides temporally with the well documented transgression and regressi

外來

Coal Correlations and Intrabasinal Subsidence: A New Analytical Perspective time periods (>10. yr) and is subject to sudden, discrete changes (or “disturbances”). A direct relationship also appears to exist between the magnitude and spatial/temporal frequency of such disturbances and the actual tectonic regime of a basin. The methodological approach outlined in this study

ACTIN

Explicate