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- W1987481523 abstract "This report contains results of the comprehensive analysis of gravity, magnetic field, and seismic data, geared to verify the geological structure of basalts in the area of study. The largest basalt deposits occur in the form of thick and extensive lava flows in Deccan plateau of the West India and in Columbia Plateau in the Cordilleras. On platforms, basalts, dolerites and diabase occur either in the form of lava sheets (plateau basalts), or as series of intrusive bodies like dikes, domes, etc. and as traps of the Siberian platform, Deccan plateau etc. Basalt exposures are characterized by hexagonal-prismatic (column-like) jointing, which becomes normal as it gets to the surface of lava cover (usually vertical, colonnade-like) or to dike contacts (in case of their steep occurrence – subhorizontal, looking like a stack of firewood). Basalts are easily identified by their columnar jointing, which looks quite spectacular, as pillars can reach enormous proportions. Side surface of basalt sheets, broken, or with prismatic jointing, reminds of a giant's causeway, paved with huge curly-stone. Column like bodies of basalts are seems to play on seismic sections below the lava coverage." @default.
- W1987481523 created "2016-06-24" @default.
- W1987481523 creator A5005926696 @default.
- W1987481523 date "2012-04-02" @default.
- W1987481523 modified "2023-09-23" @default.
- W1987481523 title "Research of Stratum of Basalts at a Site of a Shelf of India" @default.
- W1987481523 doi "https://doi.org/10.3997/2214-4609.20143714" @default.
- W1987481523 hasPublicationYear "2012" @default.
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