東華大學圖書館 |

語系: 繁體中文

說明(常見問題)

回圖書館首頁

手機版館藏查詢

登入

回首頁

切換: 標籤 | MARC模式 | ISBD

Modeling the processes that form and...

Hutton, Eric W. H.

FindBook

Google Book

Amazon

博客來

Modeling the processes that form and erode marine strata.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Modeling the processes that form and erode marine strata./
作者:	Hutton, Eric W. H.
面頁冊數:	269 p.
附註:	Source: Dissertation Abstracts International, Volume: 68-03, Section: B, page: 1518.
Contained By:	Dissertation Abstracts International68-03B.
標題:	Geophysics. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3256463

Modeling the processes that form and erode marine strata.
Hutton, Eric W. H.

Modeling the processes that form and erode marine strata. - 269 p.

Source: Dissertation Abstracts International, Volume: 68-03, Section: B, page: 1518.

Thesis (Ph.D.)--University of Colorado at Boulder, 2007.

Numerical simulators of the dynamics of strata formation of continental margins fuse information from the atmosphere, ocean and regional geology. Such models can provide information for areas and times for which actual measurements are not available, or for when purely statistical estimates are not adequate by themselves. This dissertation develops two such models that are applied to Earth's continental shelves.Subjects--Topical Terms:

535228
Geophysics.

Modeling the processes that form and erode marine strata.
LDR:03216nmm 2200301 4500 001 1835880
005 20080107105542.5
008 130610s2007 eng d
035 $a (UMI)AAI3256463
035 $a AAI3256463
040 $a UMI $c UMI
100 1 $a Hutton, Eric W. H. $3 1924499
245 1 0 $a Modeling the processes that form and erode marine strata.
300 $a 269 p.
500 $a Source: Dissertation Abstracts International, Volume: 68-03, Section: B, page: 1518.
500 $a Adviser: James P. M. Syvitski.
502 $a Thesis (Ph.D.)--University of Colorado at Boulder, 2007.
520 $a Numerical simulators of the dynamics of strata formation of continental margins fuse information from the atmosphere, ocean and regional geology. Such models can provide information for areas and times for which actual measurements are not available, or for when purely statistical estimates are not adequate by themselves. This dissertation develops two such models that are applied to Earth's continental shelves.
520 $a Sedflux is a whole margin model able to simulate the delivery of sediment and their accumulation over time scales of tens of thousands of years. The Sedflux model is extended to more realistically simulate the distributions of seafloor geotechnical parameters during the growth of a seismically active continental margin. The improved formulation better predicts the frequency, size, and location of sediment failures. Although the overall architecture is not significantly changed, the internal stratal organization is altered. Sediment failures are found to be most likely during falling or low sea-level conditions.
520 $a The Sedflux model is further extended by adding a series of new processes models, and extending the model environment to track the evolution of stratigraphy in either two or three dimensions. Additions to the 2D-mode include models that simulate (1) sediment erosion and deposition along a riverbed, (2) cross-shore transport due to ocean waves, and (3) turbidity currents and hyperpycnal flows. New processes in the 3D-mode include (1) river channel avulsion, (2) two-dimensional diffusion due to ocean storms, and (3) two-dimensional flexure due to sediment loading.
520 $a In contrast to the complex Sedflux model, a single-process model is developed that predicts the contribution of water loading to the subsidence of Earth's continental shelves. Based on a one-dimensional elastic flexure model, an analytic solution for the deflection of a linear slope, due to sea level rise and fall, is derived. This analytic solution allows a global database of deflection estimates for continental shelves, due only to increases in water loading, and the shape of the LGM continental margins. Thus, changes in eustatic sea level are disengaged from changes in relative sea level. Pleistocene variations in water loading can change the slopes of continental shelves on the order of 30%.
590 $a School code: 0051.
650 4 $a Geophysics. $3 535228
650 4 $a Physical Oceanography. $3 1019163
690 $a 0373
690 $a 0415
710 2 $a University of Colorado at Boulder. $3 1019435
773 0 $t Dissertation Abstracts International $g 68-03B.
790 1 0 $a Syvitski, James P. M., $e advisor
790 $a 0051
791 $a Ph.D.
792 $a 2007
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3256463