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- W2392296271 abstract "Studies on joint statistics,faults,folds,and focal-mechanism solution have revealed that the dip angle of the principal axis of compressive stress of the tectonic stress field in Lanzhou area since the Tertiary have gradually become steep through an alternating change from steep to gentle and vice versa,while its orientation changed from N-S,NW-SE to NW-SW.In Tertiary time,the counter-clockwise movement of the tectonic field was resulted from the counterclockwise movement of the mas-sif.In the Early-Middle Pleistocene,an important chang in style of tectonism took place in the Qing-hai-Tibet Plateau,while the Lanzhou area entered an E-W extensional tectonic deformation period.The crustal movement of the study area dominated by uplifting although the uplift was combined by horizontal movement.Every horizontal (or uplifting)movement was followed by an adjustment period, in which the crustal movement was different in style from the previous period(i.e.,when the previous period was dominated by uplifting,then horizontal movement occurred in the adjustment period and vice versa)." @default.
- W2392296271 created "2016-06-24" @default.
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- W2392296271 date "2000-01-01" @default.
- W2392296271 modified "2023-09-28" @default.
- W2392296271 title "EVOLUTIONARY CHARACTERISTICS OF THE CENOZOIC STRUCTURAL STRESS FIELD IN RHE LANZHOU AREA" @default.
- W2392296271 hasPublicationYear "2000" @default.
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