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

A test of the validity of morphometr...

University of Arkansas.

FindBook

Google Book

Amazon

博客來

A test of the validity of morphometric analysis in determining tectonic activity from ASTER derived DEMs in the Jordan-Dead Sea Transform zone.

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
正題名/作者:	A test of the validity of morphometric analysis in determining tectonic activity from ASTER derived DEMs in the Jordan-Dead Sea Transform zone./
作者:	Ata, Husam Abbas.
面頁冊數:	220 p.
附註:	Source: Dissertation Abstracts International, Volume: 69-05, Section: B, page: 2874.
Contained By:	Dissertation Abstracts International69-05B.
標題:	Geology. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3317790
ISBN:	9780549660934

A test of the validity of morphometric analysis in determining tectonic activity from ASTER derived DEMs in the Jordan-Dead Sea Transform zone.
Ata, Husam Abbas.

A test of the validity of morphometric analysis in determining tectonic activity from ASTER derived DEMs in the Jordan-Dead Sea Transform zone. - 220 p.

Source: Dissertation Abstracts International, Volume: 69-05, Section: B, page: 2874.

Thesis (Ph.D.)--University of Arkansas, 2008.

The Jordan-Dead Sea Transform (JDTZ) is an active tectonic zone which is located between the Dead Sea in the north and the Gulf of Aqaba in the south and extends approximately 245 km. The JDTZ has a complicated geomorphological setting and varied geology and it contains a number of active faults that were associated with several significant destructive earthquakes in the region. This research was initiated to develop a morphometric digital approach to examine the mountain front geomorphic form along the Jordan-Dead Sea Transform Zone to obtain intensive analysis of its potential as an indicator of seismic activity.

ISBN: 9780549660934Subjects--Topical Terms:

516570
Geology.

A test of the validity of morphometric analysis in determining tectonic activity from ASTER derived DEMs in the Jordan-Dead Sea Transform zone.
LDR:02659nam 2200289 a 45 001 854227
005 20100702
008 100702s2008 ||||||||||||||||| ||eng d
020 $a 9780549660934
035 $a (UMI)AAI3317790
035 $a AAI3317790
040 $a UMI $c UMI
100 1 $a Ata, Husam Abbas. $3 1020544
245 1 2 $a A test of the validity of morphometric analysis in determining tectonic activity from ASTER derived DEMs in the Jordan-Dead Sea Transform zone.
300 $a 220 p.
500 $a Source: Dissertation Abstracts International, Volume: 69-05, Section: B, page: 2874.
502 $a Thesis (Ph.D.)--University of Arkansas, 2008.
520 $a The Jordan-Dead Sea Transform (JDTZ) is an active tectonic zone which is located between the Dead Sea in the north and the Gulf of Aqaba in the south and extends approximately 245 km. The JDTZ has a complicated geomorphological setting and varied geology and it contains a number of active faults that were associated with several significant destructive earthquakes in the region. This research was initiated to develop a morphometric digital approach to examine the mountain front geomorphic form along the Jordan-Dead Sea Transform Zone to obtain intensive analysis of its potential as an indicator of seismic activity.
520 $a Four ASTER scenes were used as a visual digital data reference to locate geomorphic forms along the mountain fronts in the study area. Using the ASTER generated DEMs of +/-10m vertical accuracy as a base elevation reference layer, several significant mountain fronts and valley profiles were digitized using GIS technology to precisely determine their morphometric indices. The mountain front sinuosity (Smf) and the ratio of valley floor width to valley height (Vf) morphometric indices were utilized to analyze the several mountain fronts and valleys in the JDTZ to determine their tectonic activity.
520 $a The final morphometric analysis of Smf results indicated two major tectonic activity classes within the JDTZ. The active tectonic class 1 values range from 1.00 to 1.30 while the moderate to less active class 2 values are >1.30. On the other hand, the Vf analysis results suggest the existence of three tectonic activity classes. The active tectonic class 1 values range from ≤0.09 to 0.50, the moderate to less active class 2 values range from 0.51 to 1.88, and the less active (inactive) class 3 values are >1.88.
590 $a School code: 0011.
650 4 $a Geology. $3 516570
650 4 $a Physical Geography. $3 893400
650 4 $a Remote Sensing. $3 1018559
690 $a 0368
690 $a 0372
690 $a 0799
710 2 $a University of Arkansas. $3 1017562
773 0 $t Dissertation Abstracts International $g 69-05B.
790 $a 0011
791 $a Ph.D.
792 $a 2008
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3317790