Tectonic affinity of the Khanka Massif in the easternmost Central Asian Orogenic Belt: evidence from detrital zircon geochronology of Permian sedimentary rocks

Xing, Kai‐Chen; Wang, Feng; Xu, Wen‐Liang; Gao, Fuhong

doi:10.1080/00206814.2019.1619098

Cited by 10 publications

(5 citation statements)

References 85 publications

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…In this tectonic framework, the regional occurrence of similar intruand lavas and their coeval shift in magmatic nature ubiquitously around the Sea of Japan (Figure 17) can be reasonably explained without assuming imaginary strike-slip dislocation. This model is supported also by other study results (Liu et al, 2017;Tsutsumi et al, 2016;Xing et al, 2019) that confirmed a significant age cluster about 500 Ma in detrital zircon that well corresponds to the ages of detrital monazite from the Cenozoic sands, and to those of zircons from the Neoproterozoic sandstones and igneous-metamorphic rocks of South China (Gao et al, 2020;Yokoyama et al, 2010).…”

Section: Tectonic Implicationssupporting

confidence: 82%

A major change in magma sources in late Mesozoic active margin of the circum‐Sea of Japan domain: Geochemical constraints from late Paleozoic to Paleogene mafic dykes in the Sergeevka belt, southern Primorye, Russia

et al. 2021

View full text Add to dashboard Cite

More than 30 mafic dykes crop out in the Sergeevka belt in the coastal South Primorye, Far East Russia, of which geologic settings have been unclear for years. This study conducted major-and trace elements characterization, Sr-Nd isotope analyses, and Ar-Ar amphibole and U-Pb zircon datings for these rocks in order to identify their origin. The results demonstrated that all dykes are characterized by high Ba/Yb and low Nb/Y, Zr/Y, and Th/Yb ratios, which suggest their origin from arc melts derived from thin wedge mantle and shallow-dipping slab. These dykes are clearly separated into two distinct age/geochemistry suites; that is, the Paleogene and Early Cretaceous one with dolerites/basalts and adakitic rocks, and the Permian-Triassic one with high-Mg and high-Al gabbro-dolerite varieties. Their geochemistry suggests that the older suite was sourced from a primitive depleted MORB mantle (DMM)-type mantle, whereas the younger suite from an enriched mantle II (EM2)-type mantle domain. The transition in source type from DMM to EM2 occurred during the Jurassic-earliest Cretaceous time, probably by a strong influence of a mantle plume onto the long-continuing subductionrelated magmatism. The plume influence reached the maximum when the unique meimechite-picrite complex formed in the region.

show abstract

Section: Tectonic Implicationssupporting

confidence: 82%

A major change in magma sources in late Mesozoic active margin of the circum‐Sea of Japan domain: Geochemical constraints from late Paleozoic to Paleogene mafic dykes in the Sergeevka belt, southern Primorye, Russia

et al. 2021

View full text Add to dashboard Cite

show abstract

“…The sorting and processing of zircon samples for dating were completed in the laboratory of Hebei Langfang company. The target fabrication was completed by the Hubei Wuhan Shangpu company, (Wilde et al, 2000;Wu et al, 2011;Xing et al, 2020); (b) Geological map and sampling location in eastern Heilongjiang Province (Wang et al, 2015); (c) Geological map of Mishan area (Yang et al, 2015) (Ludwig, 2003). The error of analysis results and concordia ages is 1σ.…”

Section: Analysis Methodsmentioning

confidence: 99%

“…(a) schematic diagram of main tectonic units in Northeast China (Wilde et al, 2000; Wu et al, 2011; Xing et al, 2020); (b) Geological map and sampling location in eastern Heilongjiang Province (Wang et al, 2015); (c) Geological map of Mishan area (Yang et al, 2015); (d) Lithology comprehensive histogram and sampling location of Early Permian Erlongshan Formation in Mishan…”

Section: Geological Setting and Lithology Descriptionmentioning

confidence: 99%

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

Ningchen

Zhou

et al. 2022

Geological Journal

View full text Add to dashboard Cite

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.

show abstract

“…The middle potential provenances are located in the Jiamusi Massif and are composed of Cambrian to Triassic rocks (Figures 5 and 6). Source M-1 (265-240 Ma) is mainly developed in the western Jiamusi Massif and subordinately along the western part of the Mudanjiang fault [81,90,93,94,104,108,110,[119][120][121][122][123][124][125][126][127][128][129]. Source M-2 (310-265 Ma) is mostly located in the Mishan and Huanan uplifts within the Jiamusi Massif with a small amount in the Zhangguangcai Range [82,90,108,120,123,126,127,[130][131][132][133][134][135][136][137][138].…”

Section: Middle Potential Provenances (M-x)mentioning

confidence: 99%

Spatio-Temporal Evolution of the Crustal Uplift in Eastern NE China: Constraint from Detrital Zircon Ages of Late Mesozoic Clastic Rocks in the Boli Basin

Cheng

et al. 2022

Minerals

View full text Add to dashboard Cite

Detrital zircon of clastic rocks has been widely recognized as a powerful tool for the study of crustal uplift, which is of great significance for understanding multi-sphere interaction. However, young detrital zircons can only roughly constrain the depositional time of the strata, and commonly used zircon age probability density and kernel density estimations cannot provide sufficient evidence to reveal spatio-temporal differences in tectonic uplift. The basins developed in active continental margins usually contain abundant magmatic rocks, which can provide insights into basin evolution and crustal deformation when combined with sedimentary characteristics. In this study, we report detrital zircon ages of Late Mesozoic clastic rocks from the Boli Basin, being part of the Great Sanjiang Basin Group in eastern NE China, which is strongly affected by the Paleo-Pacific subduction. In conjunction with the age data of coeval magmatic rocks and potential sedimentary sources of basement rocks adjacent to the basin, the geochronologic results of this study provide solid evidence for the formation of the Boli Basin and the spatio-temporal evolution of the crustal uplift in northeastern China. The Boli Basin went through multi-phase tectonic evolution of syn-rift and post-rift stages, based on the zircon age data of clastic and igneous rocks. When the geographical distribution characteristics of potential sedimentary sources and their percentages of contribution are taken into account, two stages of eastward migration of the crustal uplift and two episodes of basin destruction caused by the tectonic extension and subsequent compression can be proposed for the Boli Basin. These processes were caused successively by the rolling back of the subducted Paleo-Pacific slab, the docking of the Okhotomorsk block along the eastern continental margin of East Asia, and the transition of the subduction zone by the collision of the Okhotomorsk block.

show abstract

Tectonic affinity of the Khanka Massif in the easternmost Central Asian Orogenic Belt: evidence from detrital zircon geochronology of Permian sedimentary rocks

Cited by 10 publications

References 85 publications

A major change in magma sources in late Mesozoic active margin of the circum‐Sea of Japan domain: Geochemical constraints from late Paleozoic to Paleogene mafic dykes in the Sergeevka belt, southern Primorye, Russia

A major change in magma sources in late Mesozoic active margin of the circum‐Sea of Japan domain: Geochemical constraints from late Paleozoic to Paleogene mafic dykes in the Sergeevka belt, southern Primorye, Russia

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

Spatio-Temporal Evolution of the Crustal Uplift in Eastern NE China: Constraint from Detrital Zircon Ages of Late Mesozoic Clastic Rocks in the Boli Basin

Contact Info

Product

Resources

About