Results 121 to 130 of about 240 (174)
Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago. [PDF]
Liu H, Sun WD, Zartman R, Tang M.
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Monitoring intercropping systems of mango in the Baikal Rift Zone
Bruno Nascimento, Camila Araujo
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Characterization of a Thermostable Endolysin of the Aeribacillus Phage AeriP45 as a Potential Staphylococcus Biofilm-Removing Agent. [PDF]
Golosova NN +7 more
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Update on Selected Topics in Acanthocephalan Parasites Research. [PDF]
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Deep structure and origin of the Baikal rift zone
Earth and Planetary Science Letters, 2006P-wave velocity images are determined under the Baikal rift zone in Siberia by using teleseismic tomography. Our results show prominent low-velocity anomalies in the upper mantle under the Baikal rift zone and high-velocity anomalies in the lithosphere under the Siberian craton.
Stephen Gao, Dapeng Zhao, Jianshe Lei
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Fractals in studies of faulting and seismicity in the Baikal rift zone
Tectonophysics, 1999Abstract Fractal analyses have been carried out for spatial patterns of faulting including over 3000 faults and seismicity of more than 60,000 earthquakes in the Baikal rift zone (BRZ). It is concluded that faulting and seismicity are in balance in the whole BRZ and out of balance in its flanks.
S.I. Sherman, A.S. Gladkov
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Baikal Rift: Active or Passive? — Comparison of the Baikal and Kenya Rift Zones
Tectonophysics, 1983Abstract The comparison of geological and geophysical data from the Kenya and Baikal rift zones permits us to consider the formation of these zones to be associated with the development of wide asthenospheric upwellings beneath them. In this sense, both rifts are active.
N.A. Logatchev +2 more
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Geodiversity and Geomorphosites of the Baikal Rift Zone
Doklady Earth SciencesShchetnikov A A +2 more
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Baikal rift zone: Structure and geodynamics
Tectonophysics, 1992Abstract The Cenozoic Baikal rift zone is superimposed on the Caledonian Baikal fold belt, representing the suture between the Precambrian Siberian craton and several microcontinents. The Baikal rift zone consists of a system of disconnected fault-bounded basins and extensional and wrench faults that straddles a major arch, having a topographic ...
N.A. Logatchev, Yu.A. Zorin
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Crustal extension in the Baikal rift zone
Tectonophysics, 1991Analysis of the gravity field along four profiles crossing the Baikal rift zone permits an estimate of the amount of anomalous mass produced by 1. (1) graben-fill sediments, 2. (2) Moho uplift and intrusion of mantle sills and dikes, 3. (3) an asthenospheric bulge.
Yu. Zorin, Lindrith Cordell
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