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

Cytology

Synorogenic Sedimentation and Subsidence in a Plio-Pleistocene Collisional Basin, Eastern Taiwann Trough south of Taiwan, which should provide a modern analog for marine deposits of the CRCB, is notably lacking in broad shallow shelf areas corresponding to widespread shallow-water facies of the Plio-Pleistocene sequence. This suggests that early stages of the collision produced less dramatic s

心胸狭窄

Institution

Sedimentary Basins in the Context of Allochthonous Terranesval with amalgamation or accretion; and 2) those that record post-amalgamation or post-accretion displacement and tectonics. Understanding terrane history prior to accretion depends primarily on recognition of latitudinally dependent magnetic, sedimentologic, and paleontologic features in the sedime

coltish

Dating Thrust-Fault Activity by Use of Foreland-Basin Stratae the Huaco sequence as a test case of various approaches to estimating thrust history..Tectonic subsidence histories, derived from well constrained stratal accumulation histories, are sensitive indicators of the thickening in the thrust belt, and are independent of local sedimentary processes. Howe

斜谷

Book 1988who wish to either stay abreast of the most recent ideas or developments or to become familiar with an important topic in the field of sedimentary geology. The series attempts to deal with sub­ jects that are in the forefront of both scientific and economic interest. The treatment of a subject in an

出生

Chris PaolaMCMC methods. The aim is to introduce and apply these techniques, thus hopefully motivating their further theoretical treatment. A few sections, mainly in Chapt978-0-387-95050-1978-1-4612-1158-7Series ISSN 0930-0325 Series E-ISSN 2197-7186

hermetic

Provenance and Sediment Dispersal in Relation to Paleotectonics and Paleogeography of Sedimentary Barustal blocks have moved as parts of mobile lithospheric plates, detritus transported from one block to another may record the times during which the two blocks were adjacent. Where orogenic belts are deeply eroded, sediment shed into nearby basins may record the former existence of rock masses remo

哀求

Isotopic Provenance of Clastic Deposits: Application of Geochemistry to Sedimentary Provenance Studicurrent and point-count studies. Although traditional basin-analysis techniques suffice in settings where there are few potential source areas, they may prove inadequate in more complex tectonic settings. In these situations isotopic analyses of whole-rock samples and mineral separates from clastic

Lasting

obstruct