Matches in SemOpenAlex for { <https://semopenalex.org/work/W2892598191> ?p ?o ?g. }
- W2892598191 endingPage "625" @default.
- W2892598191 startingPage "607" @default.
- W2892598191 abstract "In this study, Shuttle Radar Topography Mission (SRTM) Digital Elevation Model (DEM) and aeromagnetic data are used to analyse the trends of pre-existing basement structures within the Rukwa Rift Basin. The NW-trending Rukwa Rift Basin on the western branch of the East African Rift System, southwest Tanzania, is developing on the NW-trending Paleoproterozoic Ubendian orogenic belt, a belt that experienced multiple orogenic collisions associated with subduction in Proterozoic time and comprises several distinct terranes bounded by faults or shear zones. The results obtained using magnetic edge enhancement (derivatives) methods highlight major magnetic domains identified based on their distinctive magnetic patterns in relation to geology and tectonic setting of the studied area. The results also highlight the Precambrian Chisi shear zone which trends in a NW-SE direction in the subsurface, below the Lake Beds Formation sedimentary succession of the Neogene Rukwa Rift Basin. The orientation of rift border faults and other major faults and their relationship with basement fabrics inferred from SRTM DEM and magnetic data trend mainly NW-SE, which is consistent with those of the NW-trending Paleoproterozoic Ubendian orogenic belt. Thus, Paleoproterozoic Ubendian orogenic belt structures have played a significant role on geometry and orientation of the Rukwa Rift Basin. These structures facilitated strain localisation within the border faults of the rift basin by exploiting the existence of inherited lithospheric heterogeneity. It can be concluded that the pre-existing faults and shear zones define a mechanical anisotropy in the basement of the Rukwa Rift Basin and facilitated the strain localisation within the border faults of the rift." @default.
- W2892598191 created "2018-10-05" @default.
- W2892598191 creator A5016022667 @default.
- W2892598191 creator A5066761626 @default.
- W2892598191 creator A5067027839 @default.
- W2892598191 date "2019-02-01" @default.
- W2892598191 modified "2023-09-27" @default.
- W2892598191 title "The role of pre-existing Precambrian structures in the development of Rukwa Rift Basin, southwest Tanzania" @default.
- W2892598191 cites W1213685928 @default.
- W2892598191 cites W1595300053 @default.
- W2892598191 cites W1669380268 @default.
- W2892598191 cites W1895858234 @default.
- W2892598191 cites W1968094597 @default.
- W2892598191 cites W1974697134 @default.
- W2892598191 cites W1975304359 @default.
- W2892598191 cites W1976560441 @default.
- W2892598191 cites W1977029803 @default.
- W2892598191 cites W1978924057 @default.
- W2892598191 cites W1979322531 @default.
- W2892598191 cites W1980565942 @default.
- W2892598191 cites W1981543232 @default.
- W2892598191 cites W1982712732 @default.
- W2892598191 cites W1983235437 @default.
- W2892598191 cites W1987623077 @default.
- W2892598191 cites W1989563048 @default.
- W2892598191 cites W1993269300 @default.
- W2892598191 cites W1996795315 @default.
- W2892598191 cites W2000802134 @default.
- W2892598191 cites W2001485817 @default.
- W2892598191 cites W2003998383 @default.
- W2892598191 cites W2012356884 @default.
- W2892598191 cites W2012869914 @default.
- W2892598191 cites W2016134366 @default.
- W2892598191 cites W2020093204 @default.
- W2892598191 cites W2020802660 @default.
- W2892598191 cites W2022497145 @default.
- W2892598191 cites W2025592377 @default.
- W2892598191 cites W2025676217 @default.
- W2892598191 cites W2026932112 @default.
- W2892598191 cites W2027292207 @default.
- W2892598191 cites W2027447908 @default.
- W2892598191 cites W2029516467 @default.
- W2892598191 cites W2029897679 @default.
- W2892598191 cites W2038671818 @default.
- W2892598191 cites W2045329505 @default.
- W2892598191 cites W2046183881 @default.
- W2892598191 cites W2046979441 @default.
- W2892598191 cites W2047866460 @default.
- W2892598191 cites W2050840564 @default.
- W2892598191 cites W2056282404 @default.
- W2892598191 cites W2058013971 @default.
- W2892598191 cites W2059774297 @default.
- W2892598191 cites W2068161390 @default.
- W2892598191 cites W2069433376 @default.
- W2892598191 cites W2071030684 @default.
- W2892598191 cites W2072326401 @default.
- W2892598191 cites W2074093419 @default.
- W2892598191 cites W2075225778 @default.
- W2892598191 cites W2076210019 @default.
- W2892598191 cites W2076382643 @default.
- W2892598191 cites W2084744129 @default.
- W2892598191 cites W2085636637 @default.
- W2892598191 cites W2086984818 @default.
- W2892598191 cites W2091479960 @default.
- W2892598191 cites W2098891607 @default.
- W2892598191 cites W2100979625 @default.
- W2892598191 cites W2107207638 @default.
- W2892598191 cites W2108473603 @default.
- W2892598191 cites W2109599465 @default.
- W2892598191 cites W2117151033 @default.
- W2892598191 cites W2118623924 @default.
- W2892598191 cites W2122450937 @default.
- W2892598191 cites W2122975106 @default.
- W2892598191 cites W2127635502 @default.
- W2892598191 cites W2134982139 @default.
- W2892598191 cites W2146420796 @default.
- W2892598191 cites W2147299124 @default.
- W2892598191 cites W2151230758 @default.
- W2892598191 cites W2152921655 @default.
- W2892598191 cites W2154995264 @default.
- W2892598191 cites W2158819582 @default.
- W2892598191 cites W2162389023 @default.
- W2892598191 cites W2164000705 @default.
- W2892598191 cites W2165721396 @default.
- W2892598191 cites W2166134193 @default.
- W2892598191 cites W2169662270 @default.
- W2892598191 cites W2170482959 @default.
- W2892598191 cites W2178484906 @default.
- W2892598191 cites W2272975080 @default.
- W2892598191 cites W2279321587 @default.
- W2892598191 cites W2281873918 @default.
- W2892598191 cites W2294414483 @default.
- W2892598191 cites W2418381495 @default.
- W2892598191 cites W2460385708 @default.
- W2892598191 cites W2753489054 @default.
- W2892598191 cites W2767205627 @default.
- W2892598191 cites W2792759511 @default.
- W2892598191 cites W2976855724 @default.