Siberian paleomagnetic data and the problem of rigidity of the Northern Eurasian continent in the post-Paleozoic

@article{Pavlov2012SiberianPD,
  title={Siberian paleomagnetic data and the problem of rigidity of the Northern Eurasian continent in the post-Paleozoic},
  author={Vladimir Pavlov},
  journal={Izvestiya, Physics of the Solid Earth},
  year={2012},
  volume={48},
  pages={721-737}
}
  • V. Pavlov
  • Published 9 October 2012
  • Geology
  • Izvestiya, Physics of the Solid Earth
The Meso-Cenozoic paleomagnetic poles from the Siberian platform and its folded margins, which comply with the modern technical and methodological standards, are analyzed. The analysis suggests the following conclusions. (1) The geometrical relationship between the Permo-Triassic poles of the Stable Europe and Siberian Platform prohibits the possibility of relative displacements of these platforms in the post-Paleozoic time. (2) The Mesozoic paleomagnetic poles of the Siberian Platform support… 
The analysis of Meso–Cenozoic paleomagnetic poles and the apparent polar wander path of Siberia
  • A. Didenko
  • Geology
    Izvestiya, Physics of the Solid Earth
  • 2015
The Meso-Cenozoic paleomagnetic data for the Siberian Platform and its closest folded framing are analyzed for compliance with four criteria: structural-tectonic coherence, the accuracy of dating the
Palaeogeography of the Siberian platform during middle Palaeozoic Times (∼450–400 Ma): new palaeomagnetic evidence from the Lena and Nyuya rivers
New reliable palaeomagnetic data from the Siberian platform help in deciphering its palaeogeography during ∼450–400 Ma. Geochronology of late Devonian mafic sills provides time constraints for
New Late Jurassic to Early Cretaceous Paleomagnetic Results From North China and Southern Mongolia and Their Implications for the Evolution of the Mongol‐Okhotsk Suture
To better constrain the evolution of the Mongol‐Okhotsk suture, we carried out new paleomagnetic studies on Sharilyn Formation (~155 Ma) and Tsagantsav Formation (~130 Ma) in southern Mongolia,
On Time of the Triassic Rifts System Origin in Western Siberia
It is commonly believed that very large basalt volumes produced by Early Triassic magmatism had effused synchronously in both the Siberian Platform and Western Siberia in a very short time interval
Geomagnetic Secular Variations at the Permian‐Triassic Boundary and Pulsed Magmatism During Eruption of the Siberian Traps
The tempo of Large Igneous Province emplacement is crucial to determining the environmental consequences of magmatism on the Earth. Based on detailed flow‐by‐flow paleomagnetic data from the most
Correlation of the Permian-Triassic Ore-Bearing Intrusions of the Norilsk Region with the Volcanic Sequence of the Siberian Traps Based on the Paleomagnetic Data
We present detailed paleomagnetic data from the Permian-Triassic Cu-Ni-Pt–bearing intrusions of the Norilsk region (northwestern Siberian platform). Based on the analysis of geomagnetic secular
Volcanism and global environmental change
Preface List of contributors Part I. Large Volume Volcanism: Origins, Features, and Timing: 1. Large Igneous Provinces and explosive basaltic volcanism Ingrid Ukstins Peate and Linda Elkins-Tanton 2.
Paleomagnetic, Sedimentological, and Isotopic Data on Neoproterozoic Periglacial Sediments of Siberia: A New Perspective on the Low-Latitude Glaciations Problem
Abstract—Paleo- and rock magnetic, sedimentological, and isotope geochemical study is carried out for the carbonate member of Late Neoproterozoic Nichatka Formation (Siberian Platform, western slope
...
...

References

SHOWING 1-10 OF 50 REFERENCES
The Mesozoic apparent polar wander path for the Siberian domain of the Eurasian plate
Comparison of the apparent polar wander paths (APWP) is one of the most important tasks in recent paleomagnetic study. The reliability of such trajectories is largely determined by the quality and
New paleomagnetic data for the Permian-Triassic Trap rocks of Siberia and the problem of a non-dipole geomagnetic field at the Paleozoic-Mesozoic boundary
between them. Discussed in this paper are four potential factors that had caused the observed dierences between the paleomagnetic poles of Siberia and Europe: (1) the large-scale relative movements
Paleomagnetism of the Lower Cambrian from the Lower Lena River Valley: Constraints on the Apparent Polar Wander Path from the Siberian Platform and the Anomalous Behavior of the Geomagnetic Field at the Beginning of the Phanerozoic
Detailed paleomagnetic studies of Lower Cambrian reference sections of the Siberian platform were performed; the sections are located within the Chekurovka and Bulkur anticlines in the
Boreal-tethyan correlation of the Jurassic-Cretaceous boundary interval by magneto- and biostratigraphy
As a result of detail sampling and paleomagnetic study of the 27-m-thick section of Jurassic-Cretaceous boundary beds in the Nordvik Peninsula (Anabar Bay, Laptev Sea), a succession of M-zones
Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone, Siberia
SUMMARY This paper presents new data from palaeomagnetic investigations on the Upper Palaeozoic and Mesozoic geological units from the Siberian platform and the Mongol–Okhotsk suture zone. Within the
The angular velocity vectors of the main Eurasian domains in the phanerozoic and an increase in the Earth’s rotation period
Recent paleomagnetic studies and GPS-monitoring show that slow rotations of continental plates and differential rotations of separate domains inside them are important features of geophysics and
Late Jurassic-Early Cretaceous closure of the Mongol-Okhotsk Ocean demonstrated by new Mesozoic palaeomagnetic results from the Trans-Baïkal area (SE Siberia)
SUMMARY We present new palaeomagnetic results from the Transba¨ ikal area (SE Siberia), from the Mongol-Okhotsk suture zone, the boundary between the Amuria and Siberia blocks. In order to better
...
...