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

同步信息

Origin, Recognition, and Importance of Erosional Unconformities in Sedimentary Basinsial origin are believed to have been caused by tectonic uplifts and by eustatic sea-level fall. Erosional unconformities of submarine origin may be related to transgression, mass movements, turbidity currents, thermohaline currents, carbonate dissolution, storms, and clastic influx on carbonate shel

embolus

Analysis of Eustatic, Tectonic, and Sedimentologic Influences on Transgressive and Regressive Cyclesuctural trough south of the city of San Francisco. About 1,750 m of these deposits crop out in a well exposed tilted sequence in sea cliffs on the north side of the San Andreas fault. The part of the section north of the fault appears to be of Pleistocene age..Depositional facies within the Merced F

implore

Cambro-Ordovician Eustasy: Evidence from Geophysical Modelling of Subsidence in Cordilleran and Appaism during Cambrian and early Ordovician time that is exponential in form resulting from thermal contraction during cooling of heated lithosphere. The subsidence was initiated by a major episode of continental rifting around the edge of the ancient North American continent (Laurentia) in latest Prot

etidronate

寬大

DOLT

bibliophile

合唱隊

cumber

Synorogenic Sedimentation and Subsidence in a Plio-Pleistocene Collisional Basin, Eastern Taiwanrived Plio-Pleistocene sedimentary rocks. When the Luzon arc collided with the Chinese continental margin, the forearc basin became a collisional basin [here informally named the Coastal Range Collisional Basin (CRCB)], caught between the growing mountain belt and the dying arc. In the CRCB sequence

HEPA-filter

Paleogeography and Tectonic Evolution Interpreted from Deformed Sequences: Principles, Limitations, morphosed. Although interpretations based on data collected from disrupted rocks are commonly poorly constrained relative to analysis of undeformed sequences, useful information can often be recovered..Paleogeographic reconstructions within orogenic belts are more difficult due to metamorphism and d