東華大學圖書館 |

Language: English

Help

回圖書館首頁

手機版館藏查詢

Back

Switch To: Labeled | MARC Mode | ISBD

Post-glacial sedimentation in a rive...

Liu, Jing-pu.

Linked to FindBook

Google Book

Amazon

博客來

Post-glacial sedimentation in a river -dominated epicontinental shelf: The Yellow Sea example.

Record Type:	Electronic resources : Monograph/item
Title/Author:	Post-glacial sedimentation in a river -dominated epicontinental shelf: The Yellow Sea example./
Author:	Liu, Jing-pu.
Description:	151 p.
Notes:	Source: Dissertation Abstracts International, Volume: 62-10, Section: B, page: 4438.
Contained By:	Dissertation Abstracts International62-10B.
Subject:	Physical oceanography. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3029880
ISBN:	9780493422169

Post-glacial sedimentation in a river -dominated epicontinental shelf: The Yellow Sea example.
Liu, Jing-pu.

Post-glacial sedimentation in a river -dominated epicontinental shelf: The Yellow Sea example. - 151 p.

Source: Dissertation Abstracts International, Volume: 62-10, Section: B, page: 4438.

Thesis (Ph.D.)--The College of William and Mary, 2001.

This item must not be sold to any third party vendors.

The North Yellow Sea (NYS) and South Yellow Sea (SYS), stretching from the Bohai Sea in the north to the East China Sea (ECS) in the south, represents an end member of modern epicontinental seas. Because of its shallow depths, the Yellow Sea was entirely exposed subaerially during the last glacial maximum.

ISBN: 9780493422169Subjects--Topical Terms:

3168433
Physical oceanography.

Post-glacial sedimentation in a river -dominated epicontinental shelf: The Yellow Sea example.
LDR:03104nmm a2200325 4500 001 2058254
005 20150707121547.5
008 170521s2001 ||||||||||||||||| ||eng d
020 $a 9780493422169
035 $a (MiAaPQ)AAI3029880
035 $a AAI3029880
040 $a MiAaPQ $c MiAaPQ
100 1 $a Liu, Jing-pu. $3 3172186
245 1 0 $a Post-glacial sedimentation in a river -dominated epicontinental shelf: The Yellow Sea example.
300 $a 151 p.
500 $a Source: Dissertation Abstracts International, Volume: 62-10, Section: B, page: 4438.
500 $a Adviser: John D. Milliman.
502 $a Thesis (Ph.D.)--The College of William and Mary, 2001.
506 $a This item must not be sold to any third party vendors.
506 $a This item must not be added to any third party search indexes.
520 $a The North Yellow Sea (NYS) and South Yellow Sea (SYS), stretching from the Bohai Sea in the north to the East China Sea (ECS) in the south, represents an end member of modern epicontinental seas. Because of its shallow depths, the Yellow Sea was entirely exposed subaerially during the last glacial maximum.
520 $a The new post-glacial sea-level curve derived from an extensive local dataset shows a series of rapid flooding events (12--45 mm/y), separated by a series of slow rises (2--6 mm/y). By about 15 ka, sea level had reached -100 m, and seawater entered the SYS. A rapid rise during MWP-1A occurred between 14.7--14.1 ka, sea level jumped from -98 m to -74 m (40 mm/yr). At the end, the sea water had reached the southern edge of the NYS, after which sea level rose again slowly (6 mm/yr) from -72 m to -60 m. Beginning about 11.7 ka, it again jumped, from -60 m to -42 m (MWP-1B), resulting in a rapid westward flooding of the NYS. Sea level then again stagnated (between -42m to -36 m) for about 1.8 ky. Starting about 9.8 ka, the sea-level advanced again from -36m to -16 m at 9.0 ka (MWP-1C), after which most of BS, YS, and ECS had been submerged. Then another slowdown occurred between 9.0--8.0 ka when sea-level rose from -16m to -10m. The last major transgression happened between 8.1 and 7.0 ka (MWP-D), and resulted in Holocene highstand of at least +2 to 4 m along most of Chinese and Korean coastlines.
520 $a Sequence structures on this epicontinental shelf show strong landward horizontal changes, instead of the vertical changes. The first major deltaic system was developed in the NYS together with the decreased sea-level rise after MWP-1B event, and the intensified summer monsoon and subsequent increased river discharge at about 11 ka. The second subaqueous delta was built in the SYS between 9--7 ka which during another slackened sea-level after MWP-C. The modern subaqueous and subaerial deltas in the west Bahai Gulf have been formed during the sea-level highstand after the last jump of MWP-1D.
590 $a School code: 0261.
650 4 $a Physical oceanography. $3 3168433
650 4 $a Geology. $3 516570
690 $a 0415
690 $a 0372
710 2 $a The College of William and Mary. $3 1018629
773 0 $t Dissertation Abstracts International $g 62-10B.
790 $a 0261
791 $a Ph.D.
792 $a 2001
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3029880