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                             12 gevonden resultaten
nr titel auteur tijdschrift jaar jaarg. afl. pagina('s) type
1 Evaluation of the Metastability in Nanodispersed Heterophase Titanomagnetites Afremov, L. L.

58 6 p. 969-980
artikel
2 Features of Frictional Melting of Rocks and Melt Crystallization in a Seismic Process: Case Study of Pseudotachylites of the Ladoga Region Matveev, M. A.

58 6 p. 902-928
artikel
3 Integral Formula for Solving the Thermal Conjugation Problem for Layered Media: the Structure of the Integral Operator Ladovskii, I. V.

58 6 p. 941-956
artikel
4 Laboratory Study on Frictional Behavior of Rock Blocks of Meter Scale. Methods and Preliminary Results Kocharyan, G. G.

58 6 p. 929-940
artikel
5 Mantle Structure and Processes in Transition Zone of the Baikal Rift Zone Vinnik, L. P.

58 6 p. 773-781
artikel
6 Metachronous Remagnetization of the Ordovician Rocks of Moyero River Key Section (Northern Siberian Platform): Duration and Probable Mechanism Pavlov, V. E.

58 6 p. 815-841
artikel
7 On the Calculation of the Fundamental Green’s Affinor for a Field in Layered Medium with Uniaxial Electric and Magnetic Anisotropy Based on the V.I. Dmitriev’s Method Kevorkyants, S. S.

58 6 p. 957-968
artikel
8 Palaeomagnetism of the Sarmatian-Maeotian of the Eastern Paratethys: Remagnetization or Not? Salnaia, N. V.

58 6 p. 882-901
artikel
9 Paleomagnetism of the Silurian and Devonian Thicknesses of Southern and Central Tuva Kovalenko, D. V.

58 6 p. 782-814
artikel
10 Properties of Thermochemical Remanent Magnetization on Basalt Samples Containing Titanomagnetites with Increased Thermal Stability Gribov, S. K.

58 6 p. 842-858
artikel
11 Taylor Polynomial Spatial Reference Field Method for Field Geomagnetic Diurnal Variation Reduction Su, Shupeng

58 6 p. 981-991
artikel
12 Ultra-Low Geomagnetic Field Intensity in the Mesoproterozoic Based on the Dike Complex Rocks of the Bunger Oasis (1133 Ma, East Antarctica) Shcherbakova, V. V.

58 6 p. 859-881
artikel
                             12 gevonden resultaten
 
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