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- W2035491797 abstract "Neotectonic influence has conditioned the development of the Moa and Ipixuna fluvial belts in the southwestern Brazilian Amazon region. The area underwent a compressive tectonics with reverse N–S fault dipping to the west that formed an “en échelon system” system from west to east, from the Serras do Divisor ranges to the Jurua river. As a response to stress, subsiding blocks with NW–SE trends were developed. The E–W to N55° W topographic trends could represent transcurrent dextral transtensional faults. Width of alluvial belts increases along the sequence of “en échelon system” blocks. Correlated with the increase of width, the quantity of channels formed by avulsion increases as well. The Moa and Ipixuna alluvial belts, respectively reaching ca. 9 and 7 km maximum width, are “abnormally” wide because they developed in subsiding blocks stretched in a NW–SE trend. Fluvial dynamics was dominated by avulsion in the subsiding blocks during the late Pleistocene and, probably, during part of the Holocene." @default.
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- W2035491797 date "2000-10-01" @default.
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- W2035491797 title "Neotectonic influence on tropical rivers of southwestern Amazon during the late quaternary: the Moa and Ipixuna river basins, Brazil" @default.
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- W2035491797 doi "https://doi.org/10.1016/s1040-6182(00)00022-7" @default.
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