語系:
繁體中文
English
說明(常見問題)
回圖書館首頁
手機版館藏查詢
登入
回首頁
到查詢結果
[ subject:"Earth Sciences, general." ]
切換:
標籤
|
MARC模式
|
ISBD
Evolution of karst in the lower part...
~
Temovski, Marjan.
FindBook
Google Book
Amazon
博客來
Evolution of karst in the lower part of Crna Reka River Basin
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Evolution of karst in the lower part of Crna Reka River Basin/ by Marjan Temovski.
作者:
Temovski, Marjan.
出版者:
Cham :Springer International Publishing : : 2016.,
面頁冊數:
xiii, 265 p. :ill., map, digital ;24 cm.
內容註:
Introduction -- General overview of the research area -- Methodology -- Hypogenic cave development -- Epigenic cave development -- Characteristics of karst surface -- General conclusions -- Appendix A -- Appendix B.
Contained By:
Springer eBooks
標題:
Karst - Macedonia. -
電子資源:
http://dx.doi.org/10.1007/978-3-319-24547-8
ISBN:
9783319245478$q(electronic bk.)
Evolution of karst in the lower part of Crna Reka River Basin
Temovski, Marjan.
Evolution of karst in the lower part of Crna Reka River Basin
[electronic resource] /by Marjan Temovski. - Cham :Springer International Publishing :2016. - xiii, 265 p. :ill., map, digital ;24 cm. - Springer theses,2190-5053. - Springer theses..
Introduction -- General overview of the research area -- Methodology -- Hypogenic cave development -- Epigenic cave development -- Characteristics of karst surface -- General conclusions -- Appendix A -- Appendix B.
This thesis addresses karst development in a terrain characterized by a highly complex geological and geomorphological evolution. It tackles the extent and complexity of both epigenic and hypogenic karst development, based on morphological analyses of caves, combined with analyses and datations of cave sediments and their correlation to regional geological and geomorphological evolution. Hypogenic karst registered is mainly the result of hydrothermal speleogenesis due to increased geothermal gradient in connection with nearby Pliocene-Pleistocene volcanic centers, with occurrence of sulfuric acid speleogenesis and ghost-rock weathering due to local geological or lithological control. Epigenic speleogenesis is strongly controlled by base level oscillations, with also examples of deep phreatic (now fossil) caves connected to regional base level rise, and per-ascensum speleogenesis. Another important finding is the constraining of the timing of Mariovo Lake draining in the Pleistocene, an important event in order to understand the geomorphological evolution in Macedonia, as it led to the onset of fluvial development and incision of valleys, shaping most of the present morphology.
ISBN: 9783319245478$q(electronic bk.)
Standard No.: 10.1007/978-3-319-24547-8doiSubjects--Topical Terms:
2179581
Karst
--Macedonia.
LC Class. No.: GB600.4.M33
Dewey Class. No.: 551.447094976
Evolution of karst in the lower part of Crna Reka River Basin
LDR
:02421nmm a2200325 a 4500
001
2028904
003
DE-He213
005
20160726165548.0
006
m d
007
cr nn 008maaau
008
160908s2016 gw s 0 eng d
020
$a
9783319245478$q(electronic bk.)
020
$a
9783319245454$q(paper)
024
7
$a
10.1007/978-3-319-24547-8
$2
doi
035
$a
978-3-319-24547-8
040
$a
GP
$c
GP
041
0
$a
eng
050
4
$a
GB600.4.M33
072
7
$a
RB
$2
bicssc
072
7
$a
SCI019000
$2
bisacsh
082
0 4
$a
551.447094976
$2
22
090
$a
GB600.4.M33
$b
T281 2016
100
1
$a
Temovski, Marjan.
$3
2179580
245
1 0
$a
Evolution of karst in the lower part of Crna Reka River Basin
$h
[electronic resource] /
$c
by Marjan Temovski.
260
$a
Cham :
$b
Springer International Publishing :
$b
Imprint: Springer,
$c
2016.
300
$a
xiii, 265 p. :
$b
ill., map, digital ;
$c
24 cm.
490
1
$a
Springer theses,
$x
2190-5053
505
0
$a
Introduction -- General overview of the research area -- Methodology -- Hypogenic cave development -- Epigenic cave development -- Characteristics of karst surface -- General conclusions -- Appendix A -- Appendix B.
520
$a
This thesis addresses karst development in a terrain characterized by a highly complex geological and geomorphological evolution. It tackles the extent and complexity of both epigenic and hypogenic karst development, based on morphological analyses of caves, combined with analyses and datations of cave sediments and their correlation to regional geological and geomorphological evolution. Hypogenic karst registered is mainly the result of hydrothermal speleogenesis due to increased geothermal gradient in connection with nearby Pliocene-Pleistocene volcanic centers, with occurrence of sulfuric acid speleogenesis and ghost-rock weathering due to local geological or lithological control. Epigenic speleogenesis is strongly controlled by base level oscillations, with also examples of deep phreatic (now fossil) caves connected to regional base level rise, and per-ascensum speleogenesis. Another important finding is the constraining of the timing of Mariovo Lake draining in the Pleistocene, an important event in order to understand the geomorphological evolution in Macedonia, as it led to the onset of fluvial development and incision of valleys, shaping most of the present morphology.
650
0
$a
Karst
$z
Macedonia.
$3
2179581
650
1 4
$a
Earth Sciences.
$3
642591
650
2 4
$a
Earth Sciences, general.
$3
1001754
710
2
$a
SpringerLink (Online service)
$3
836513
773
0
$t
Springer eBooks
830
0
$a
Springer theses.
$3
1314442
856
4 0
$u
http://dx.doi.org/10.1007/978-3-319-24547-8
950
$a
Earth and Environmental Science (Springer-11646)
筆 0 讀者評論
館藏地:
全部
電子資源
出版年:
卷號:
館藏
1 筆 • 頁數 1 •
1
條碼號
典藏地名稱
館藏流通類別
資料類型
索書號
使用類型
借閱狀態
預約狀態
備註欄
附件
W9276168
電子資源
11.線上閱覽_V
電子書
EB GB600.4.M33 T281 2016
一般使用(Normal)
在架
0
1 筆 • 頁數 1 •
1
多媒體
評論
新增評論
分享你的心得
Export
取書館
處理中
...
變更密碼
登入