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- W2019293510 abstract "Abstract The Garm polygon is confined to the junction between Tien-Shan and the Peter the Great fault zone separating the Pamirs and Tien-Shan. It is just in the zone of contact between the fault zone itself and Tien-Shan (the spurs of the Gissar ridge) that a submeridional overthrust of the fault zone on the Gissar block is revealed along the surface inclined to the horizontal by an angle of 40°, the velocity of the overthrust being approximately 20–25 mm/yr. Recently the area of the polygon has been increased. Investigations over the expanded polygon permit the preliminary conclusion that alongside the overthrust mentioned above there is a block in the fault zone approaching southwesterly along the contact with the Gissar block. Attempts are made to enlarge the deformational network so as to cover the fault zone completely." @default.
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- W2019293510 date "1979-02-01" @default.
- W2019293510 modified "2023-09-27" @default.
- W2019293510 title "Surface deformation over the Garm geodynamic polygon" @default.
- W2019293510 doi "https://doi.org/10.1016/0040-1951(79)90226-9" @default.
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