This chapter discusses the cyclicity of the mesozoic sedimentation on the eastern margin of the Chinese craton as a response to the main geodynamic events in the adjacent active oceanic area. Mesozoic volcano-sedimentary deposits of the Sikhote-Alin have been sufficiently well studied, but they were considered separately for the eastern margin of the Chinese Craton and for the intensively dislocated mountain Sikhote-Alin, situated more eastward. As a result, synchronous Mesozoic events have not been compared and correlated. In this chapter, such an attempt has been undertaken. The main structural elements of the Sea of Japan region and transition zone between the Chinese ancient craton on the west and the marginal seas of the western Pacific on the east are shown in the chapter. It examines the way the development of these two enormous geological structures have acted reciprocally during the Mesozoic and the way the events in the tectonically active, mobile eastern area influenced the epiplatform sedimentary processes on the eastern extremity of the stable Chinese Craton.
V. V. Yarmolyuk合作论文数3
Nikolay Bortnikov合作论文数Department of Mineralogy, Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of Sciences3M. I. Kuz’min合作论文数2IV Murav'eva合作论文数2ID Ryabchikov合作论文数2V. I. Kazansky合作论文数2LS Borodin合作论文数2
Aleksey A. Kotov合作论文数Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences2
F. A. Letnikov合作论文数2
Sergey Alexeevich Marakushev合作论文数2Yu. G. Safonov合作论文数2Andrei V. Girnis合作论文数2
O. A. Bogatikov合作论文数Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry Staromonetnyi per. 35, Russian Academy of Sciences2
Alexander V. Sobolev合作论文数Institut Science De La Terre, University of Grenoble Alpes;Institute of Earth Sciences, Université Joseph Fourier;Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences2V. N. Kholodov合作论文数2D. V. Grichuk合作论文数2B. I. Omel’yanenko合作论文数2V. A. Glebovitskii合作论文数2
V. Yu. Prokofiev合作论文数2DV Rundqvist合作论文数1A. V. Samsonov合作论文数1N. N. Laverov合作论文数1A. M. Kozlovskyi合作论文数1V. S. Antipin合作论文数1S. P. Korikovskii合作论文数1V. S. Samoilov合作论文数1н л добрецов合作论文数1
I.V. Chernyshev合作论文数Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences1Sv Ruzhentsev合作论文数1
Alexey Travin合作论文数VS Sobolev Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences1P. V. Markevich合作论文数1
Victor Vinograd合作论文数Theoretical Geochemistry Program;Institute of Earth Sciences;Uppsala University;Institute of Earth Sciences, Uppsala University1N. P. Laverov合作论文数1Yu. M. Pushcharovsky合作论文数1
Igor' V. Kemkin合作论文数1
Sergey Petrovic. Korikovsky合作论文数1
A. V. Nikiforov合作论文数1Vladimir B. Naumov合作论文数1Nikolai V Vladykin合作论文数Vinogradov Institute of Geochemistry, Russian Academy of Sciences1Yu. B. Shapovalov合作论文数1
Yuri D. Zakharov合作论文数1
Irina a Andreeva合作论文数Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry Staromonetnyi per. 35, Russian Academy of Sciences1
M. V. Borisov合作论文数OOO Nanotekh1
Leonid Danyushevsky合作论文数Centre of Excellence in Ore Deposits, University of Tasmania;School of Earth Sciences, University of Tasmania1Yu. D. Zakharov合作论文数1V. F. Polin合作论文数1
Igor S. Puchtel合作论文数Department of Geology, University of Maryland1
Alexander G Simakin合作论文数Russian Academy of Sciences Institute of Experimental Mineralogy Chernogolovka1Pavel V. Markevich合作论文数Institute of Solid-State and Semiconductor Physics ul. Brovki, Belarussian Academy of Sciences1
