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 geological and geophysical study o...

McCall, Curtis William.

FindBook

Google Book

Amazon

博客來

A geological and geophysical study of the 1929 Grand Banks slide.

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
正題名/作者:	A geological and geophysical study of the 1929 Grand Banks slide./
作者:	McCall, Curtis William.
面頁冊數:	230 p.
附註:	Source: Masters Abstracts International, Volume: 45-04, page: 1909.
Contained By:	Masters Abstracts International45-04.
標題:	Geology. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=MR23855
ISBN:	9780494238554

A geological and geophysical study of the 1929 Grand Banks slide.
McCall, Curtis William.

A geological and geophysical study of the 1929 Grand Banks slide. - 230 p.

Source: Masters Abstracts International, Volume: 45-04, page: 1909.

Thesis (M.Sc.)--Saint Mary's University (Canada), 2006.

The St. Pierre Slope off the Grand Banks of Newfoundland is the site of a large submarine failure complex that was the result of the 1929 Grand Banks earthquake. A 2000 km2 area has been investigated in detail using seismic reflection, sidescan sonar and core data. Failure development and evolution is strongly influenced by local changes in gradient on the slope. Documented modes of failure are mass flows, slumps, and isolated occurrences of glides and creep. The total volume of sediment involved in initial failure is estimated at 93 km3: 47 km3 as MTDs on the slope and 46 km3 that evacuated, likely contributing to the 1929 turbidity current. The total volume of the turbidite is conservatively estimated at 175 km3, suggesting that at least 222 km 3 (47 km3 + 175 km3) of sediment was eroded and displaced during the 1929 event.

ISBN: 9780494238554Subjects--Topical Terms:

516570
Geology.

A geological and geophysical study of the 1929 Grand Banks slide.
LDR:01608nam 2200253 a 45 001 967478
005 20110915
008 110915s2006 eng d
020 $a 9780494238554
035 $a (UMI)AAIMR23855
035 $a AAIMR23855
040 $a UMI $c UMI
100 1 $a McCall, Curtis William. $3 1291351
245 1 2 $a A geological and geophysical study of the 1929 Grand Banks slide.
300 $a 230 p.
500 $a Source: Masters Abstracts International, Volume: 45-04, page: 1909.
502 $a Thesis (M.Sc.)--Saint Mary's University (Canada), 2006.
520 $a The St. Pierre Slope off the Grand Banks of Newfoundland is the site of a large submarine failure complex that was the result of the 1929 Grand Banks earthquake. A 2000 km2 area has been investigated in detail using seismic reflection, sidescan sonar and core data. Failure development and evolution is strongly influenced by local changes in gradient on the slope. Documented modes of failure are mass flows, slumps, and isolated occurrences of glides and creep. The total volume of sediment involved in initial failure is estimated at 93 km3: 47 km3 as MTDs on the slope and 46 km3 that evacuated, likely contributing to the 1929 turbidity current. The total volume of the turbidite is conservatively estimated at 175 km3, suggesting that at least 222 km 3 (47 km3 + 175 km3) of sediment was eroded and displaced during the 1929 event.
590 $a School code: 1104.
650 4 $a Geology. $3 516570
650 4 $a Geophysics. $3 535228
690 $a 0372
690 $a 0373
710 2 0 $a Saint Mary's University (Canada). $3 1020608
773 0 $t Masters Abstracts International $g 45-04.
790 $a 1104
791 $a M.Sc.
792 $a 2006
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=MR23855