The Riphean-Vendian-Cambrian sedimentogenesis zone at the southeastern margin of the North Asian Craton: The geostructural setting and regionalization

2011 ◽  
Vol 5 (5) ◽  
pp. 433-445 ◽  
Author(s):  
V. G. Varnavsky ◽  
V. E. Kuznetsov
Keyword(s):  
North Asian Craton ◽  
The North ◽  
Southeastern Margin

Late mesozoic adakite volcanism of the Ugan volcanic structure (Southeastern Margin of the North Asian Craton): 40Ar/39Ar geochronological and geochemical evidence

2012 ◽  
Vol 445 (2) ◽  
pp. 947-950 ◽  
Author(s):  
A. A. Sorokin ◽  
A. P. Sorokin ◽  
V. A. Ponomarchuk ◽  
Yu. A. Martynov ◽  
A. M. Larin ◽  
...  
Keyword(s):  
Volcanic Structure ◽  
North Asian Craton ◽  
Late Mesozoic ◽  
Geochemical Evidence ◽  
The North ◽  
Southeastern Margin

New 40Ar/39Ar age of granitic rocks and related gold mineralization at the Kirovskoye deposit (southeastern margin of the North Asian craton)

2014 ◽  
Vol 458 (2) ◽  
pp. 1230-1235 ◽  
Author(s):  
A. A. Sorokin ◽  
A. V. Ponomarchuk ◽  
A. V. Travin ◽  
V. A. Ponomarchuk ◽  
K. D. Vakhtomin
Keyword(s):  
Gold Mineralization ◽  
Granitic Rocks ◽  
North Asian Craton ◽  
The North ◽  
Southeastern Margin

Tectonics and metallogeny of the junction zone between the North Asian craton and Pacific tectonic belt

2016 ◽  
Vol 10 (1) ◽  
pp. 13-27
Author(s):  
M. V. Goroshko ◽  
B. F. Shevchenko ◽  
V. A. Guryanov ◽  
G. Z. Gil’manova
Keyword(s):  
Junction Zone ◽  
North Asian Craton ◽  
The North ◽  
Tectonic Belt

scholarly journals South Anyui suture: tectono-stratigraphy, deformations, and principal tectonic events

2009 ◽  
Vol 4 ◽  
pp. 201-221 ◽  
Author(s):  
S. D. Sokolov ◽  
G. Ye. Bondarenko ◽  
P. W. Layer ◽  
I. R. Kravchenko-Berezhnoy
Keyword(s):  
Active Continental Margin ◽  
Strike Slip ◽  
Passive Margin ◽  
The South ◽  
Asian Continent ◽  
Oblique Collision ◽  
North Asian Craton ◽  
The North ◽  
Continental Block ◽  
South Anyui Suture

Abstract. Geochronologic and structural data from the terranes of the South Anyui suture zone record a protracted deformational history before, during and after an Early Cretaceous collision of the passive margin of the Chukotka-Arctic Alaska continental block with the active continental margin of the North Asian continent. Preceding this collision, the island arc complexes of the Yarakvaam terrane on the northern margin of the North Asian craton record Early Carboniferous to Neocomian ages in ophiolite, sedimentary, and volcanic rocks. Triassic to Jurassic amphibolites constrain the timing of subduction and intraoceanic deformation along this margin. The protracted (Neocomian to Aptian) collision of the Chukotka passive margin with the North Asian continent is preserved in a range of structural styles including first north verging folding, then south verging folding, and finally late collisional dextral strike slip motions which likely record a change from orthogonal collision to oblique collision. Due to this collision, the southern passive margin of Chukotka was overthrust by tectonic nappes composed of tectono-stratigraphic complexes of the South Anyui terrane. Greenschists with ages of 115–119 Ma are related to the last stages of this collision. The postcollisional orogenic stage (Albian to Cenomanian) is characterized by sinistral strike slip faults and an extensional environment.

The petrochemistry of the Lower Proterozoic metamorphic rocks from the Dabieshan-Lianyungang area, the southeastern margin of the North China Platform

1991 ◽  
Vol 55 (379) ◽  
pp. 263-276 ◽  
Author(s):  
Sang Longkang
Keyword(s):  
Continental Margin ◽  
North China ◽  
Active Continental Margin ◽  
The South ◽  
North China Platform ◽  
The North ◽  
Lower Proterozoic ◽  
Southeastern Margin ◽  
Tectonic Settings ◽  
North China Plate

AbstractBased on geological studies, 141 rock analyses and 5 trace element analyses of metabasites, the present paper deals with the rock association, chemical features, protolith formation and the original tectonic settings upwards through the Lower Proterozoic metamorphic strata in the Dabieshan-Lianyungang area, in the south-east of the North China Platform. The results of the study indicate that the lower and middle parts of the metamorphic strata comprise terrigenous clastics, phosphoritic and aluminous sedimentary formations which formed under stable continental margin conditions. In the middle-upper part a calc-alkaline volcano-sedimentary formation under the active continental margin was developed. The Lower Proterozoic meta-strata of sedimentary-volcanosedimentary origin from bottom upwards suggest that the tectonic evolution of the south-eastern margin of the North China Platform is a process from stabilization to mobilization. This process suggests a northward subduction of the Yangtze Plate under the North China Plate during the later part of the early Proterozoic.

scholarly journals Repositioning the Great Unconformity at the southeastern margin of the North China Craton

2019 ◽  
Vol 324 ◽  
pp. 1-17 ◽  
Author(s):  
Bin Wan ◽  
Qing Tang ◽  
Ke Pang ◽  
Xiaopeng Wang ◽  
Zhian Bao ◽  
...  
Keyword(s):  
North China Craton ◽  
North China ◽  
The North ◽  
Southeastern Margin
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