NDLI: Geologic structure of Western Primorye: Structuring dynamics

Please wait, while we are loading the content...

Stratigraphy of the Oligocene-Miocene boundary sediments in the Nezhinsky brown coal field (Primorye) and the problem of the Paleogene-Neogene boundary in the region

Development of lacustrine-boggy sedimentary environments in the ancient Rasshua Island caldera (Central Kuril Islands) in the Holocene

Russian Journal of Pacific Geology : Volume 6, Issue 3, May 2012

Russian Journal of Pacific Geology : Volume 6, Issue 2, April 2012

Russian Journal of Pacific Geology : Volume 6, Issue 1, February 2012

Russian Journal of Pacific Geology : Volume 5

Russian Journal of Pacific Geology : Volume 4

Russian Journal of Pacific Geology : Volume 3

Russian Journal of Pacific Geology : Volume 2

Russian Journal of Pacific Geology : Volume 1

Geologic structure of Western Primorye: Structuring dynamics

Content Provider	Springer Nature Link
Author	Nevolin, P. L. Utkin, V. P. Mitrokhin, A. N. Kutub Zade, T. K.
Copyright Year	2012
Abstract	The first data are reported on the structuring dynamics of Western Primorye. The analysis of the structural parageneses of the least studied macro- and mesolevels of the arrangement of the geologic space allowed us to distinguish three sequentially superposed structural patterns (parageneses), each of which was formed by its own stress field during separate geodynamic periods: the Late Proterozoic-Early Paleozoic, the Middle-Late Paleozoic, and the Mesozoic-Cenozoic. During the first two episodes of geodynamic activation (Late Proterozoic-Early Paleozoic), the main compression axis was oriented longitudinally. The first episode was characterized by the formation of a thrust-fold structural pattern. The second episode resulted in the superposition of the meridional riftogenic structures and, respectively, in the pull-apart normal-fault segmentation of the crystalline basement into mainly longitudinal blocks, which partially coincide with the previously distinguished terranes. During the latitudinal compression and oblate deformation that predominanted during the Middle-Late Paleozoic geodynamic period, the down-thrown and uplifted blocks were transformed into depressions and arches, respectively. The depressions were filled with Paleozoic sediments, while the primary rocks in the arches experienced granitization with the formation of two granitic complexes that joined terranes. The granites are characterized by shadow and shear-type fold and pseudofolded forms. The Mesozoic-Cenozoic period governed by NNW compression is divided into the Triassic-Jurassic, Early Cretaceous, and Tertiary tectonic episodes. During the Triassic-Jurassic period, the ENE-trending narrow arches and depressions were formed by warping. The arches accumulated granitized rocks, while the depressions were compensated for by the Early-Late Triassic sedimentary-volcanogenic sediments. All these processes led to the formation of structural complexes that joined and overlapped older complexes of meridional blocks (terranes) across the strike. Two subsequent Mesozoic-Cenozoic episodes manifested themselves in the discrete formation of coal-bearing depressions due to the NNW compression and ENE extension of the warping products.
Starting Page	275
Ending Page	293
Page Count	19
File Format	PDF
ISSN	18197140
Journal	Russian Journal of Pacific Geology
Volume Number	6
Issue Number	4
e-ISSN	18197159
Language	English
Publisher	SP MAIK Nauka/Interperiodica
Publisher Date	2012-08-16
Publisher Place	Dordrecht
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	structuring dynamics structural parageneses stress fields geodynamic periods Western Primorye Far East Geology
Content Type	Text
Resource Type	Article
Subject	Geology Geophysics Geochemistry and Petrology Oceanography Paleontology Stratigraphy

Sl.	Authority	Responsibilities	Communication Details
1	Ministry of Education (GoI), Department of Higher Education	Sanctioning Authority	https://www.education.gov.in/ict-initiatives
2	Indian Institute of Technology Kharagpur	Host Institute of the Project: The host institute of the project is responsible for providing infrastructure support and hosting the project	https://www.iitkgp.ac.in
3	National Digital Library of India Office, Indian Institute of Technology Kharagpur	The administrative and infrastructural headquarters of the project	Dr. B. Sutradhar bsutra@ndl.gov.in
4	Project PI / Joint PI	Principal Investigator and Joint Principal Investigators of the project	Dr. B. Sutradhar bsutra@ndl.gov.in Prof. Saswat Chakrabarti will be added soon
5	Website/Portal (Helpdesk)	Queries regarding NDLI and its services	support@ndl.gov.in
6	Contents and Copyright Issues	Queries related to content curation and copyright issues	content@ndl.gov.in
7	National Digital Library of India Club (NDLI Club)	Queries related to NDLI Club formation, support, user awareness program, seminar/symposium, collaboration, social media, promotion, and outreach	clubsupport@ndl.gov.in
8	Digital Preservation Centre (DPC)	Assistance with digitizing and archiving copyright-free printed books	dpc@ndl.gov.in
9	IDR Setup or Support	Queries related to establishment and support of Institutional Digital Repository (IDR) and IDR workshops	idr@ndl.gov.in

Shear structural paragenesis and its role in continental rifting of the East Asian margin

The system of Cenozoic depressions in the Amur and Primorye regions: The structure, tectonic position, and geodynamic interpretation

The Ust-Davydovka Formation: A paleogene reference stratigraphic unit of the Primorye region, Russian Far East

Role of latitudinal compression in the formation of Paleozoic intrusive structures in the southern Primorye region in the Far East

Hypotheses of the brown loam formation in the Primorye region (Russian Far East): Hindsight and the new view

The Tafuinsky granite massif, southern Primorye region: The structures and geodynamics of longitudinal compression

Late Paleozoic and Mesozoic deformations in the southwestern Primorye region

Hydrothermal precious opals of the Raduzhnoe deposit, north Primorye: The nature of the opalescence

First evidence for the Middle Triassic volcanism in South Primorye

Geologic structure of Western Primorye: Structuring dynamics

Similar Documents

Shear structural paragenesis and its role in continental rifting of the East Asian margin

The system of Cenozoic depressions in the Amur and Primorye regions: The structure, tectonic position, and geodynamic interpretation

The Ust-Davydovka Formation: A paleogene reference stratigraphic unit of the Primorye region, Russian Far East

Role of latitudinal compression in the formation of Paleozoic intrusive structures in the southern Primorye region in the Far East

Hypotheses of the brown loam formation in the Primorye region (Russian Far East): Hindsight and the new view

The Tafuinsky granite massif, southern Primorye region: The structures and geodynamics of longitudinal compression

Late Paleozoic and Mesozoic deformations in the southwestern Primorye region

Hydrothermal precious opals of the Raduzhnoe deposit, north Primorye: The nature of the opalescence

First evidence for the Middle Triassic volcanism in South Primorye

Geologic structure of Western Primorye: Structuring dynamics