skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View a record

Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.

Please search for material in iDiscover for up-to-date information about the library collection.


Record #129281:

Fluctuations of lakes and their environments since last glaciation in Amdo area, Tibet / Yongping Shen, Daoming Xu.

Title: Fluctuations of lakes and their environments since last glaciation in Amdo area, Tibet / Yongping Shen, Daoming Xu.
Author(s): Shen, Yongping.
Xu, Daoming.
Date: 1994.
Language: Chinese.
In: Journal of Glaciology and Geocryology. (1994.), Vol. 16(2) (1994)
Abstract: Describes these lakes, both in tectonic glaciated basins. May have existed only since 35 ka BP. Underlying strata is formed of Tertiary fluvial and lacustrine sediments with glacial deformational structures.
Notes:

Journal of Glaciology and Geocryology. Vol. 16(2) :173-180 (1994).

English abstract, p.179-180.

Keywords: 551.33 -- Glacial geology.
551.332.24 -- Glacio-fluvial deposits.
551.332.26 -- Glacio-lacustrine deposits and varves.
551.333 -- Glacial deformation and glaciotectonic structures.
556.55 -- Lakes and ponds.
E7 -- Glaciology: glacial geology and ice ages.
(515) -- Tibet.
SPRI record no.: 129281

MARCXML

LDR 01308naa#a2200000#a#4500
001 SPRI-129281
005 20240328124842.0
007 ta
008 240328s1994####xx#a##|##|###|0||#0|chi#d
035 ## ‡aSPRI-129281
040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡achi
100 1# ‡aShen, Yongping.
245 10 ‡aFluctuations of lakes and their environments since last glaciation in Amdo area, Tibet /‡cYongping Shen, Daoming Xu.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1994.
300 ## ‡ap. 173-180 :‡bdiags., tables.
500 ## ‡aJournal of Glaciology and Geocryology. Vol. 16(2) :173-180 (1994).
500 ## ‡aEnglish abstract, p.179-180.
520 3# ‡aDescribes these lakes, both in tectonic glaciated basins. May have existed only since 35 ka BP. Underlying strata is formed of Tertiary fluvial and lacustrine sediments with glacial deformational structures.
546 ## ‡aIn Chinese.
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332.24 -- Glacio-fluvial deposits.‡2udc
650 07 ‡a551.332.26 -- Glacio-lacustrine deposits and varves.‡2udc
650 07 ‡a551.333 -- Glacial deformation and glaciotectonic structures.‡2udc
650 07 ‡a556.55 -- Lakes and ponds.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(515) -- Tibet.‡2udc
700 1# ‡aXu, Daoming.
773 0# ‡7nnas ‡tJournal of Glaciology and Geocryology. ‡gVol. 16(2) (1994) ‡wSPRI-72888
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240328