• Corpus ID: 202169412

LA-ICP-MS zircon U-Pb dating of the Upper Carboniferous volcanic rocks from northern Beishan region in Gansu Province and its tectonic significance

@article{Yazhu2013LAICPMSZU,
  title={LA-ICP-MS zircon U-Pb dating of the Upper Carboniferous volcanic rocks from northern Beishan region in Gansu Province and its tectonic significance},
  author={Niu Ya-zhu},
  journal={Geological bulletin of China},
  year={2013},
  url={https://api.semanticscholar.org/CorpusID:202169412}
}
  • Niu Ya-zhu
  • Published 2013
  • Geology
  • Geological bulletin of China
Much information remains to be discovered concerning the Late Paleozoic ocean-land transition in Beishan region. The Late Paleozoic strata can provide important evidence for this subject. However, the research on the age of the upper Carboniferous volcanic rocks from northern Beishan region is insufficient. This paper shows that the LA-ICP-MS zircon U-Pb ages of the "Early Carboniferous Baishan Formation" from Heiyinghsan area are 308.6Ma ±1.0Ma and 299.1Ma ±2.4Ma, which belong to the Late… 
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5 Citations

5 Citations

Permo‐Carboniferous crustal accretion in the northern Beishan Orogen, Inner Mongolia: Constraints from Sr–Nd–Hf isotopes and zircon U–Pb geochronology of diorites and granitoids

To research the Late Palaeozoic accretionary orogeny and vertical crustal accretion in the northern Beishan Orogen, the zircon U–Pb age, zircon Hf, and whole‐rock Sr–Nd isotopic composition from the…

Tectonic evolution of the Beishan orogen in central Asia: Subduction, accretion, and continent-continent collision during the closure of the Paleo-Asian Ocean

The Beishan orogen is part of the Neoproterozoic to early Mesozoic Central Asian Orogenic System in central Asia that exposes ophiolitic complexes, passive-margin strata, arc assemblages, and…

Unconformity-bounded Upper Paleozoic megasequences in the Beishan Region (NW China) and implications for the timing of the Paleo-Asian Ocean closure

Late Palaeozoic Tectonic Evolution of the Northern Part of the Zhusileng‐Hangwula Arc in the Middle Segment of the Central Asian Orogenic Belt: Insights From Structural Geology and Geochronology

The final closure time and tectonic evolution of the middle segment of the Paleo‐Asian Ocean (PAO) remain poorly constrained. The northern part of the Zhusileng‐Hangwula arc, located in the middle…

Timing and Style of Final Closure of the Paleo‐Asian Ocean: Perspectives From the Big Geodata Analysis and Machine Learning Model

The Paleo‐Asian Ocean (PAO), was located between the Siberian Craton and the Tarim‐North China Craton, and its subduction‐closure history are important for studying the evolution of the Central Asian…