A new terrane subdivision for Mongolia: implications for the Phanerozoic crustal growth of Central Asia

2002 ◽  
Vol 21 (1) ◽  
pp. 87-110 ◽  
Author(s):  
Gombosuren Badarch ◽  
W Dickson Cunningham ◽  
Brian F Windley
Keyword(s):  
Central Asia ◽  
Crustal Growth

Petrogenesis of Early-Permian sanukitoids from West Junggar, Northwest China: Implications for Late Paleozoic crustal growth in Central Asia

2015 ◽  
Vol 662 ◽  
pp. 385-397 ◽  
Author(s):  
Jiyuan Yin ◽  
Wen Chen ◽  
Wenjiao Xiao ◽  
Chao Yuan ◽  
Min Sun ◽  
...  
Keyword(s):  
Central Asia ◽  
Northwest China ◽  
Late Paleozoic ◽  
Crustal Growth ◽  
Early Permian ◽  
West Junggar

Paleozoic crustal growth and metallogeny of Central Asia: evidence from magmatic-hydrothermal ore systems of Central Kazakhstan

2000 ◽  
Vol 328 (1-2) ◽  
pp. 69-87 ◽  
Author(s):  
J Heinhorst ◽  
B Lehmann ◽  
P Ermolov ◽  
V Serykh ◽  
S Zhurutin
Keyword(s):  
Central Asia ◽  
Crustal Growth

The Tectonics of the Altaids: Crustal Growth During the Construction of the Continental Lithosphere of Central Asia Between ∼750 and ∼130 Ma Ago

2018 ◽  
Vol 46 (1) ◽  
pp. 439-494 ◽  
Author(s):  
A.M. Celâl Şengör ◽  
Boris A. Natal'in ◽  
Gürsel Sunal ◽  
Rob van der Voo
Keyword(s):  
High Resolution ◽  
Central Asia ◽  
Continental Crust ◽  
Growth Rates ◽  
Siberian Craton ◽  
Geochemical Data ◽  
Crustal Growth ◽  
Continental Lithosphere ◽  
Mountain Belt ◽  
Time Period

The largest mountain belt in Central Asia (∼9 million km2) is called the Altaids. It was assembled between ∼750 and ∼130 Ma ago around the western and southern margins of the Siberian Craton, partly on an older collisional system (the “Urbaykalides”). Geological, geophysical, and geochemical data—mostly high-resolution U-Pb ages—document the growth of only three arc systems in Central and Northwest Asia during this time period, an interval throughout which there were no major arc or continental collisions in the area. While the Altaids were being constructed as a Turkic-type orogen, continental crust grew in them by 1/3 of the global total. The Altaids thus added some 3 million km2to the continental crust over a period of 0.6 billion years, typical of Phanerozoic crustal growth rates.

Crustal growth stages in the Songino block of the early caledonian superterrane in Central Asia: II. Geochemical and Nd-isotope data

Petrology ◽  
2013 ◽  
Vol 21 (5) ◽  
pp. 409-426 ◽  
Author(s):  
V. P. Kovach ◽  
I. K. Kozakov ◽  
E. B. Salnikova ◽  
V. V. Yarmolyuk ◽  
A. M. Kozlovsky ◽  
...  
Keyword(s):  
Central Asia ◽  
Growth Stages ◽  
Crustal Growth ◽  
Nd Isotope ◽  
Isotope Data

Crustal growth stages in the Songino block of the Early Caledonian superterrane in Central Asia: I. Geological and geochronological data

Petrology ◽  
2013 ◽  
Vol 21 (3) ◽  
pp. 203-220 ◽  
Author(s):  
I. K. Kozakov ◽  
E. B. Sal’nikova ◽  
V. V. Yarmolyuk ◽  
V. P. Kovach ◽  
A. M. Kozlovskii ◽  
...  
Keyword(s):  
Central Asia ◽  
Growth Stages ◽  
Crustal Growth ◽  
Geochronological Data

Precambrian detrital zircons in the Early Paleozoic Chinese Altai: Their provenance and implications for the crustal growth of central Asia

2011 ◽  
Vol 189 (1-2) ◽  
pp. 140-154 ◽  
Author(s):  
Yingde Jiang ◽  
Min Sun ◽  
Guochun Zhao ◽  
Chao Yuan ◽  
Wenjiao Xiao ◽  
...  
Keyword(s):  
Central Asia ◽  
Detrital Zircons ◽  
Crustal Growth ◽  
Early Paleozoic

The Phanerozoic Continental Crustal Growth in Central Asia and the Evolution of Laurasia Supercontinent

2001 ◽  
Vol 4 (4) ◽  
pp. 632-633 ◽  
Author(s):  
Dawei Hong ◽  
Wang Shiguang ◽  
Xie Xilin ◽  
Zhang Jisheng
Keyword(s):  
Central Asia ◽  
Crustal Growth
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