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
切換:
標籤
|
MARC模式
|
ISBD
Volcanic Stratigraphy and Lithogeoch...
~
Glendenning, Michael W. P., Jr.
FindBook
Google Book
Amazon
博客來
Volcanic Stratigraphy and Lithogeochemistry of the Northern Section of the Lynn Lake Greenstone Belt: Implications for Regional Geodynamics and Metallogenesis.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Volcanic Stratigraphy and Lithogeochemistry of the Northern Section of the Lynn Lake Greenstone Belt: Implications for Regional Geodynamics and Metallogenesis./
作者:
Glendenning, Michael W. P., Jr.
面頁冊數:
296 p.
附註:
Source: Masters Abstracts International, Volume: 54-01.
Contained By:
Masters Abstracts International54-01(E).
標題:
Geology. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1569024
ISBN:
9781321341126
Volcanic Stratigraphy and Lithogeochemistry of the Northern Section of the Lynn Lake Greenstone Belt: Implications for Regional Geodynamics and Metallogenesis.
Glendenning, Michael W. P., Jr.
Volcanic Stratigraphy and Lithogeochemistry of the Northern Section of the Lynn Lake Greenstone Belt: Implications for Regional Geodynamics and Metallogenesis.
- 296 p.
Source: Masters Abstracts International, Volume: 54-01.
Thesis (M.A.Sc.)--University of Windsor (Canada), 2015.
This item must not be sold to any third party vendors.
The MacLellan Au-Ag deposit, located in the Paleoproterozoic Lynn Lake greenstone belt of the Trans-Hudson Orogen, Manitoba, is hosted by a package of plagioclase-amphibole, chlorite-amphibole, and quartz-plagioclase-biotite schists that are considered to be representative of the geodynamic evolution of the northern section of the Lynn Lake greenstone belt. A combination of field and petrographic observations and high-precision trace element chemistry have identified the protoliths to the host rock sequence as transitional aluminous basalt with subordinate picrite and biotite-altered aluminous basalt, respectively. The Th-Nb-La-REE systematics of these rocks are consistent with a rifted continental margin environment. Volcanic rocks with similar Th-Nb-La-REE systematics to those from the MacLellan host rock sequence have been identified throughout the Lynn Lake region. Therefore, it is proposed that the Lynn Lake greenstone belt represents a rifted continental margin and based on this revised geodynamic model, the mineral potential of the belt should be reassessed.
ISBN: 9781321341126Subjects--Topical Terms:
516570
Geology.
Volcanic Stratigraphy and Lithogeochemistry of the Northern Section of the Lynn Lake Greenstone Belt: Implications for Regional Geodynamics and Metallogenesis.
LDR
:02204nmm a2200313 4500
001
2060564
005
20150831100034.5
008
170521s2015 ||||||||||||||||| ||eng d
020
$a
9781321341126
035
$a
(MiAaPQ)AAI1569024
035
$a
AAI1569024
040
$a
MiAaPQ
$c
MiAaPQ
100
1
$a
Glendenning, Michael W. P., Jr.
$3
3174733
245
1 0
$a
Volcanic Stratigraphy and Lithogeochemistry of the Northern Section of the Lynn Lake Greenstone Belt: Implications for Regional Geodynamics and Metallogenesis.
300
$a
296 p.
500
$a
Source: Masters Abstracts International, Volume: 54-01.
500
$a
Advisers: Joel E. Gagnon; Ali Polat.
502
$a
Thesis (M.A.Sc.)--University of Windsor (Canada), 2015.
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 MacLellan Au-Ag deposit, located in the Paleoproterozoic Lynn Lake greenstone belt of the Trans-Hudson Orogen, Manitoba, is hosted by a package of plagioclase-amphibole, chlorite-amphibole, and quartz-plagioclase-biotite schists that are considered to be representative of the geodynamic evolution of the northern section of the Lynn Lake greenstone belt. A combination of field and petrographic observations and high-precision trace element chemistry have identified the protoliths to the host rock sequence as transitional aluminous basalt with subordinate picrite and biotite-altered aluminous basalt, respectively. The Th-Nb-La-REE systematics of these rocks are consistent with a rifted continental margin environment. Volcanic rocks with similar Th-Nb-La-REE systematics to those from the MacLellan host rock sequence have been identified throughout the Lynn Lake region. Therefore, it is proposed that the Lynn Lake greenstone belt represents a rifted continental margin and based on this revised geodynamic model, the mineral potential of the belt should be reassessed.
590
$a
School code: 0115.
650
4
$a
Geology.
$3
516570
650
4
$a
Geochemistry.
$3
539092
650
4
$a
Plate tectonics.
$3
542702
690
$a
0372
690
$a
0996
690
$a
0592
710
2
$a
University of Windsor (Canada).
$b
Earth Sciences.
$3
3174734
773
0
$t
Masters Abstracts International
$g
54-01(E).
790
$a
0115
791
$a
M.A.Sc.
792
$a
2015
793
$a
English
856
4 0
$u
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1569024
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
W9293222
電子資源
11.線上閱覽_V
電子書
EB
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