Book contents
- Frontmatter
- Contents
- List of contributors
- Preface
- 1 Major global change: framework for the modern world
- 2 Carboniferous-to-Triassic evolution of the Panthalassan margin in southern South America
- 3 Permian and Triassic geologic events in Sonora, northwestern Mexico
- 4 Advances in the correlation of the Permian
- 5 Examples of late Hercynian transtensional tectonics in the Southern Alps (Italy)
- 6 Succession of selected bioevents in the continental Permian of the Southern Alps (Italy): improvements in intrabasinal and interregional correlations
- 7 Permian chronostratigraphic subdivisions and events in China
- 8 Indosinian Tectogeny in the geological correlation of Vietnam and adjacent regions
- 9 Sitsa flora from the Permian of South Primorye
- 10 Late Permian bimodal volcanism in South Primorye
- 11 Syngenetic and epigenetic mineral deposits in Permian and Triassic sequences of the Primorye region
- 12 The mid-Permian: major changes in geology, environment, and faunas and some evolutionary implications
- 13 Variations in the disappearance patterns of rugosan corals in Tethys and their implications for environments at the end of the Permian
- 14 Fluctuations in pelagic environments near the Permian–Triassic boundary in the Mino-Tamba Terrane, southwest Japan
- 15 Late Changxingian ammonoids, bivalves, and brachiopods in South Primorye
- 16 Radiolaria from Permian–Triassic boundary beds in cherty deposits of Primorye (Sikhote-Alin)
- 17 Early Mesozoic magmatism in the Russian Far East
- 18 Transgressive conodont faunas of the early Triassic: an opportunity for correlation in the Tethys and the circum-Pacific
- 19 Triassic biostratigraphy and palaeobiogeography of East Asia
- 20 Classification and correlation of Triassic limestones in Sikhote-Alin on the basis of corals
- 21 Evolution of the platform elements of the conodont genus Metapolygnathus and their distribution in the Upper Triassic of Sikhote-Alin
- 22 Late Triassic North American halobiid bivalves: diversity trends and circum-Pacific correlations
- 23 Upper Triassic Chinle Group, Western United States: a nonmarine standard for late Triassic time
- 24 Otapirian Stage: its fauna and microflora
- 25 Upper Palaeozoic glaciation and Carboniferous and Permian faunal changes in Argentina
- Index
10 - Late Permian bimodal volcanism in South Primorye
Published online by Cambridge University Press: 13 October 2009
- Frontmatter
- Contents
- List of contributors
- Preface
- 1 Major global change: framework for the modern world
- 2 Carboniferous-to-Triassic evolution of the Panthalassan margin in southern South America
- 3 Permian and Triassic geologic events in Sonora, northwestern Mexico
- 4 Advances in the correlation of the Permian
- 5 Examples of late Hercynian transtensional tectonics in the Southern Alps (Italy)
- 6 Succession of selected bioevents in the continental Permian of the Southern Alps (Italy): improvements in intrabasinal and interregional correlations
- 7 Permian chronostratigraphic subdivisions and events in China
- 8 Indosinian Tectogeny in the geological correlation of Vietnam and adjacent regions
- 9 Sitsa flora from the Permian of South Primorye
- 10 Late Permian bimodal volcanism in South Primorye
- 11 Syngenetic and epigenetic mineral deposits in Permian and Triassic sequences of the Primorye region
- 12 The mid-Permian: major changes in geology, environment, and faunas and some evolutionary implications
- 13 Variations in the disappearance patterns of rugosan corals in Tethys and their implications for environments at the end of the Permian
- 14 Fluctuations in pelagic environments near the Permian–Triassic boundary in the Mino-Tamba Terrane, southwest Japan
- 15 Late Changxingian ammonoids, bivalves, and brachiopods in South Primorye
- 16 Radiolaria from Permian–Triassic boundary beds in cherty deposits of Primorye (Sikhote-Alin)
- 17 Early Mesozoic magmatism in the Russian Far East
- 18 Transgressive conodont faunas of the early Triassic: an opportunity for correlation in the Tethys and the circum-Pacific
- 19 Triassic biostratigraphy and palaeobiogeography of East Asia
- 20 Classification and correlation of Triassic limestones in Sikhote-Alin on the basis of corals
- 21 Evolution of the platform elements of the conodont genus Metapolygnathus and their distribution in the Upper Triassic of Sikhote-Alin
- 22 Late Triassic North American halobiid bivalves: diversity trends and circum-Pacific correlations
- 23 Upper Triassic Chinle Group, Western United States: a nonmarine standard for late Triassic time
- 24 Otapirian Stage: its fauna and microflora
- 25 Upper Palaeozoic glaciation and Carboniferous and Permian faunal changes in Argentina
- Index
Summary
The effects of the late Permian volcanism in Primorye are evident primarily along the southern margin of the Khanka Massif, a crystalline massif representing the extreme eastern block of the Sino-Korean Platform. Volcanism developed there under a variety of geodynamic conditions. In the western part of South Primorye, Upper Permian volcanics and associated terrigenous and carbonaceous rocks settled in the sea basin, which was formed through the destruction of the ancient sialic basement by the Hercynian orogenic movement. When that orogenesis was completed, that depression turned into a foldbelt, which is mapped as the West Primorye (or Khasan-Grodekovo) structuralfacies zone (Nazarenko and Bazhanov, 1987).
In the eastern part of South Primorye, Upper Permian volcanic rocks formed under the platform conditions directly on the area of the Khanka Massif in separate volcano-tectonic depressions. Their occurrence immediately on the ancient Precambrian rocks shows that they and accompanying terrigenous deposits belong to the complex of the platform mantle.
This chapter describes the structure and composition of the Upper Permian volcanogenic complex of South Primorye.
Position and structure of the volcanogenic complex
The Upper Permian volcanogenic formation is best studied in the West Primorye Fold Zone. It is a marginal eastern member of the meridional Laoelin-Grodekovo Depression, which wedges from the south to the Sino-Korean Platform, covering the adjacent territories in Korea and China (Smirnov, 1963). Deep faults outline the depression and separate it from ancient western and eastern crystalline massifs.
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- Information
- Late Palaeozoic and Early Mesozoic Circum-Pacific Events and their Global Correlation , pp. 106 - 108Publisher: Cambridge University PressPrint publication year: 1997
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