Geochronology and geochemistry of early Paleozoic intrusive rocks from the Khanka Massif in the Russian Far East: Petrogenesis and tectonic implications

Xu, Ting; Xu, Wen‐Liang; Wang, Feng; Ge, Wen‐Chun; Сорокин, А. А.

doi:10.1016/j.lithos.2017.12.004

Cited by 26 publications

(13 citation statements)

References 57 publications

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“…And a time span of 25 Ma was recognized as late Pan-African in the Jiamusi massif . In addition, similar ages were also reported in the Jiamusi-Khanka massif, with ε Hf (t) values ranging from negative to positive (Bi et al, 2014(Bi et al, , 2017Luan et al, 2017;Xu et al, 2018). The Cambrian detrial zircons from the Nanshuangyashan Formation show variable ε Hf (t) values (−16.5 to +1.4) (Fig.…”

Section: Cambrian Magmatic Event and Late Pan-african Eventsupporting

confidence: 72%

“…These age groups have been widely reported as magmatic events in the Jiamusi-Khanka and Songnen massif, including from gabbro, diorite, plagiogranite, granodiorite, monzogranite, graphic granite, alkali feldspar granite, and associated volcanic rocks, with zircon U-Pb ages from 296 Ma to 244 Ma (Wu et al, , 2002Huang et al, 2008;Wei, 2012;Yu et al, 2013aYu et al, , 2013bBi et al, 2014Bi et al, , 2015Bi et al, , 2016Bi et al, , 2017Pu et al, 2015;Sun et al, 2015;Dong et al, 2017b;Meng et al, 2008;Xu et al, 2012). In the Jiamusi-Khanka massif, these include the Liulian granodiorite (284±2 Ma) and hornblende-gabbro The zircon ε Hf (t) were cited from Cao et al, 2011;Yu et al, 2013a;Bi et al, 2014Bi et al, , 2015Bi et al, , 2016Bi et al, , 2017Yang et al, 2015;Luan et al, 2017;Xu et al, 2018. CAOB = Central Asian Orogenic Belt; YFTB = Yanshan Fold-and-Thrust Belt (Yang et al, 2006).…”

Section: Early Permian To Early Triassic Magmatic Eventsmentioning

confidence: 99%

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Detrital Zircon U‐Pb Dating of Nanshuangyashan Formation in the Jiamusi Massif, NE China and its Tectonic Implications

Cui

Zeng

Zhang

et al. 2019

Acta Geologica Sinica (Eng)

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A suite of the fossil-rich marine-land interbedded strata (Nanshuangyashan Formation) is distributed at the eastern margin of the Jiamusi massif in the eastern Heilongjiang Province, NE China. The authors had recently discovered a suite of arkose beneath the marine-land interbedded strata, which overlays unconformably on the Permain granite in the eastern margin of the Jiamusi massif. The LA-ICP-MS zircon U-Pb dating indicate that all detrital zircons from the analysed four arkose samples show the four population ages of ＞800 Ma, 538-481 Ma, 269-250 Ma and 223-215 Ma. The former three population ages are widely recorded in the Jiamusi-Khanka massif and the Songnen massif. The later group is the minimal age population in the analyzed samples, limiting the sedimentation time of the arkoses occurred after the Late Triassic. At present, the minimal age population is not recorded in the Jiamusi massif, but the granites with the ages of 228-210 Ma are widely distributed in the Songnen-Zhangguangcai Range massif and the Khanka massif. The predominantly Permian zircons are characterized by oscillatory zoning and euhedral shapes, with variable zircon ε Hf (t) values (−5.5 to +11.2), indicating that they were derived from mixture sources, possibly mixed with components of the Songnen-Zhangguangcai Range massif and the Jiamusi-Khanka massif. These results, combined with regional analyses, indicate that the closing of Mudanjiang ocean and Panthalassa ocean possibly existed from Early Permian to Late Triassic.

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Section: Cambrian Magmatic Event and Late Pan-african Eventsupporting

confidence: 72%

Section: Early Permian To Early Triassic Magmatic Eventsmentioning

confidence: 99%

Detrital Zircon U‐Pb Dating of Nanshuangyashan Formation in the Jiamusi Massif, NE China and its Tectonic Implications

Cui

Zeng

Zhang

et al. 2019

Acta Geologica Sinica (Eng)

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“…Thus, early Neoproterozoic rocks are the oldest known basement in this united block. The more widespread but younger basement shared by the three blocks is formed by late Pan‐African (~500 Ma; Wilde, Dorsett‐Bain, & Liu, ; Wilde, Zhang, & Wu, , Wilde, Wu, & Zhang, ) granulite and early Palaeozoic granitoids (Tsutsumi, Yokoyama, Kasatkin, & Golozubov, ; T. Xu, Xu, Wang, Ge, & Sorokin, ). Palaeozoic sedimentary cover was deposited along the eastern margin of the Jiamusi and the Khanka blocks, including Early Palaeozoic marbles, non‐marine terrigenous rocks, and late Palaeozoic volcano–sedimentary strata (Khanchuk et al, ; Meng et al, ; Yang, Ge, Zhao, Yu, & Zhang, ; F. Q. Zhang, Chen, et al, ; X.…”

Section: Geological Backgroundmentioning

confidence: 99%

“…Z. Zhang, Guo, et al, ). Some N‐S trending late Permian to Early Triassic granitoids intruded into the western Jiamusi and Khanka blocks (Huang et al, ; K. Liu, Zhang, Wilde, Zhou, et al, ; Wu, Wilde, & Sun, ; T. Xu et al, ; Yang et al, ), whereas the Late Triassic to Early Jurassic magmatic rocks are exposed rarely in the Jiamusi Block but extensively in the western Bureya and Khanka blocks (K. Liu, Zhang, Wilde, Zhou, et al, ; Ma, Zhu, Zhou, & Qiao, ; Sorokin et al, ; Sorokin, Kudryashov, & Kotov, ; Sorokin, Ovchinnikov, Kudryashov, & Sorokina, ; Yang et al, ). The late Early Cretaceous magmatism, including a ~100‐Ma basalt‐andesite‐dacite association, is widespread in the Jiamusi Block (M. D. Sun et al, ).…”

Section: Geological Backgroundmentioning

confidence: 99%

“…J. Xu, Xu, et al, 2013) Figure 2, respectively). High-grade orthogneisses exposed in the southern Jiamusi Block yield zircon U-Pb ages of 898-891 Ma (Yang et al, 2017) & Liu, 1997;Wilde, Zhang, & Wu, 2000, Wilde, Wu, & Zhang, 2003 granulite and early Palaeozoic granitoids (Tsutsumi, Yokoyama, Kasatkin, & Golozubov, 2014;T. Xu, Xu, Wang, Ge, & Sorokin, 2018).…”

Section: Continental Blocksmentioning

confidence: 99%

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Zircon U–Pb dating and whole‐rock geochemistry of volcanic rocks in eastern Heilongjiang Province, NE China: Implications for the tectonic evolution of the Mudanjiang and Paleo‐Pacific oceans from the Jurassic to Cretaceous

Wilde

Zhang

et al. 2019

Geological Journal

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The eastern Heilongjiang Province, NE China, is located in the eastern CAOB (Central Asian Orogenic Belt). Previous studies suggest that subduction of the Mudanjiang and Paleo‐Pacific oceans had been initiated in this area during the early Mesozoic. However, research on the Mesozoic volcanic rocks is insufficient, limiting our understanding of the relationship between magmatism and subduction process. To solve the problem, seven volcanic rocks in the Lesser Xing'an‐Zhangguangcai Range and the Jiamusi Block were collected for zircon U–Pb dating (SHRIMP) and whole‐rock geochemical analysis. Most samples from the Lesser Xing'an‐Zhangguangcai Range are Jurassic in age (189–178 Ma), including andesite, trachyandesite, trachydacite, and rhyolite. The andesitic to trachytic rocks were generated by magma mixing at an active continental margin, whereas the rhyolite is highly fractionated I‐type. All the samples from the Jiamusi Block and one basaltic andesite from the Lesser Xing'an Range are late Early Cretaceous in age (ca. 100 Ma) and were formed in a back‐arc extensional setting (roll‐back). Fractional crystallization was important in the generation of most Cretaceous rocks (basalt to trachydacite). However, magma mixing or crustal contamination was required to explain some andesites from the Jiamusi Block showing extremely low Cr, Ni, and Mg#. When integrated with the coeval blueschist‐facies metamorphism, the Early Jurassic volcanism indicates an active continental margin in the Lesser Xing'an‐Zhangguangcai Range due to the westward subduction of the Mudanjiang Ocean. After the closure of the Mudanjiang Ocean, two NE/NNE trending sinistral strike‐slip faults in NE China were triggered, accompanied by the slab roll‐back of the Paleo‐Pacific oceanic plate. The Jurassic continental arc and accretionary complexes in NE China were cut through by the two strike‐slip faults and bended to form small oroclines. At ca. 100 Ma, numerous accretionary complexes were accreted along the eastern margin of the CAOB, further forcing the retreat of trench and slab roll‐back. The late Early Cretaceous intra‐continental volcanism was generated in the Lesser Xing'an‐Zhangguangcai Range and Jiamusi Block during this roll‐back process.

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The Early Permian assembly of the Jiamusi Massif and Khanka Massif: Evidence from sediment sources

Ningchen

Zhou

et al. 2022

Geological Journal

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The Jiamusi-Khanka Massif is an important tectonic unit of the Central Asian Orogenic Belt in North-east China. Its Late Palaeozoic tectonic properties and the timing of assembly have restricted the understanding of the tectonic evolution process at the eastern segment of the Central Asian Orogenic Belt for a long time. Based on the study of clastic rock petrology and zircon U-Pb chronology of the Early Permian Erlongshan Formation in Mishan, it is clear that the zircon age of the Early Permian Erlongshan Formation in Mishan is mainly Late Palaeozoic, with a major age peak at 300 ± 3 Ma and secondary age peaks at 356 ± 7 Ma and 475 ± 10 Ma.The provenance mainly comes from the magmatic arc source area, and Early Palaeozoic (500-420 Ma) detrital zircons mainly come from the south-east margin of Jiamusi Massif, Late Palaeozoic (400-270 Ma) detrital zircons mainly come from the eastern margin of Jiamusi Massif and the northern margin of Khanka Massif.Among them, detrital zircons of a special age group 330-310 Ma come from the north of Khanka Massif, while 490-470 Ma detrital zircons which are common in the Early-Middle Permian strata of Khanka Massif come from Jiamusi Massif. Combined with the evidence of petrology and palaeontology, this paper believes that the Early Permian Jiamusi Massif and Khanka Massif should be a unified Massif, that is, Jiamusi-Khanka Massif.

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Geochronology and geochemistry of early Paleozoic intrusive rocks from the Khanka Massif in the Russian Far East: Petrogenesis and tectonic implications

Cited by 26 publications

References 57 publications

Detrital Zircon U‐Pb Dating of Nanshuangyashan Formation in the Jiamusi Massif, NE China and its Tectonic Implications

Detrital Zircon U‐Pb Dating of Nanshuangyashan Formation in the Jiamusi Massif, NE China and its Tectonic Implications

Zircon U–Pb dating and whole‐rock geochemistry of volcanic rocks in eastern Heilongjiang Province, NE China: Implications for the tectonic evolution of the Mudanjiang and Paleo‐Pacific oceans from the Jurassic to Cretaceous

The Early Permian assembly of the Jiamusi Massif and Khanka Massif: Evidence from sediment sources

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