NDLI: Evolution and deep structure of the Zeya-Bureya and Songliao sedimentary basins (East Asia)

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

Evolution and deep structure of the Zeya-Bureya and Songliao sedimentary basins (East Asia)

Content Provider	Springer Nature Link
Author	Sorokin, A. P. Malyshev, Yu. F. Kaplun, V. B. Sorokina, A. T. Artemenko, T. V.
Copyright Year	2013
Abstract	The evolution and deep structure of the Songliao and Zeya-Bureya basins can be divided into the rift, platform (subsidence), and neotectonic phases. The rift phase (Middle Jurassic-Early Cretaceous) climaxed at the formation of a basin-wide near N-S-oriented rift system, which was followed (Late Cretaceous) by the deposition of the deep-water organic-rich lacustrine source facies with the maximum thickness identified in the Songliao basin (up to 1100 m). The neotectonic phase was marked by the pronounced differences in the basin’s development caused by the formation of a series of E-W-trending transverse structures, which eventually separated the basins, changed the drainage pattern, and blocked the rivers draining southwards from the Zeya-Bureya to the Songliao basin.The differences in the deep structure of the basins are also strongly pronounced. High heat flow values of more than 70 mW/m$^{2}$ are typical of the Songliao basin, and its mantle heat flow component is higher than the crustal one, as compared to the Zeya-Bureya basin (below 50 mW/m$^{2}$). The crustal thickness of the Zeya-Bureya basin is higher than that of the Songliao basin (38–42 km and 29–34 km) with a lithospheric thickness of 110–140 km and 50–75 km, respectively. The only exception is the southern Zeya-Bureya basin, which has an electrical structure similar to that of the Songliao basin.These differences have important implications for the evaluation of the hydrocarbon potential of the rift basins. It was suggested that the evaluation of the hydrocarbon potential of the sedimentary basins or parts of these basins should account for two factors: (1) the influence of the lithospheric motions and the related collisional processes and (2) the anomalies in the deep lithospheric structures (the high heat flow and the reduced crustal and lithospheric thickness). The results of this study indicate that the southern part of the Zeya-Bureya basin (in particular, the Lermontovka, Dmitrievka, Mikhailovka, Ekaterinoslavka, and Arkhara troughs) is interpreted to have a fairly high hydrocarbon potential.
Starting Page	77
Ending Page	91
Page Count	15
File Format	PDF
ISSN	18197140
Journal	Russian Journal of Pacific Geology
Volume Number	7
Issue Number	2
e-ISSN	18197159
Language	English
Publisher	SP MAIK Nauka/Interperiodica
Publisher Date	2013-04-17
Publisher Place	Dordrecht
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	rift platform neotectonic phases crust lithosphere heat flow conductivity hydrocarbon potential the Zeya-Bureya and Songliao basins 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

Geoelectric section of the lithosphere of the Amur-Zeya sedimentary basin deduced from magnetotelluric soundings

Palynoflora of the Gil’chin and Dim dinosaur localities (the Zeya-Bureya Basin, Russian Far East)

Geological and geophysical interpretation of the detailed geophysical data on the Lower Zeya region of the Zeya-Bureya sedimentary basin

Space geodesy in geodynamic studies: Recent movements in the Zeya-Bureya Basin

Geoelectric section of the lithosphere of the Amur-Zeya sedimentary basin deduced from magnetotelluric sounding along the Blagoveshchensk-Birakan profile

Comparison of geodynamic models and the hydrocarbon potential of sedimentary basins in the Russian Far East and SE Asia

Structure and evolution of the Sunwu-Jiayin basin in NE China and its relation to the Zeya-Bureya basin in the Far East of Russia

Cretaceous stage in the evolution of the Jiamusi-Bureya fragment of the continental margin as exemplified by the Bureya and Hegang basins

Mesozoic sandstones and the reconstruction of tectonic depositional environments in the Bureya sedimentary basin in the Far East

Evolution and deep structure of the Zeya-Bureya and Songliao sedimentary basins (East Asia)

Similar Documents

Geoelectric section of the lithosphere of the Amur-Zeya sedimentary basin deduced from magnetotelluric soundings

Palynoflora of the Gil’chin and Dim dinosaur localities (the Zeya-Bureya Basin, Russian Far East)

Geological and geophysical interpretation of the detailed geophysical data on the Lower Zeya region of the Zeya-Bureya sedimentary basin

Space geodesy in geodynamic studies: Recent movements in the Zeya-Bureya Basin

Geoelectric section of the lithosphere of the Amur-Zeya sedimentary basin deduced from magnetotelluric sounding along the Blagoveshchensk-Birakan profile

Comparison of geodynamic models and the hydrocarbon potential of sedimentary basins in the Russian Far East and SE Asia

Structure and evolution of the Sunwu-Jiayin basin in NE China and its relation to the Zeya-Bureya basin in the Far East of Russia

Cretaceous stage in the evolution of the Jiamusi-Bureya fragment of the continental margin as exemplified by the Bureya and Hegang basins

Mesozoic sandstones and the reconstruction of tectonic depositional environments in the Bureya sedimentary basin in the Far East

Evolution and deep structure of the Zeya-Bureya and Songliao sedimentary basins (East Asia)