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• W2017030390 endingPage "1407" @default.
• W2017030390 startingPage "1387" @default.
• W2017030390 abstract "The positions of certain nonmarine sedimentary basins in central and southern Alaska are spatially related to the geometry of adjacent curved faults. These interior basins occur along the northern, convex side of these fault systems which change trend from northwest in Canada and eastern Alaska to east‐west in central Alaska and to northeast in western Alaska. The basins probably initiated in early to middle Tertiary time and deposition within all basins continued through the Quaternary, broadly synchronous with Tertiary strike‐slip displacements along the Tintina, Denali, and Border Ranges fault systems. We examine the spatial and temporal relationship between basins and faults by using a mechanical model of curved strike‐slip faults based on boundary elements. We relate slip along the curved faults to Tertiary Pacific‐North American plate motions by using principal stress directions inferred from the plate motion directions. Locations of the predicted mean stress reductions around the fault bends caused by fault slip correlate well with positions of the interior basins. Our results suggest that basin subsidence and location were controlled primarily by the geometry of adjacent curved fault systems and the state of stress in Alaska during the Tertiary. Mechanical interaction between curved Alaskan fault systems increases the tendency for basin subsidence. Stresses inferred from early Tertiary plate motion vectors are not oriented correctly to drive right lateral slip along Kaltag, Farewell, and parallel faults in western Alaska. Furthermore, these stress states would have produced left lateral displacements, for which there is no evidence, along these western faults in their present orientations. We find that a combination of slightly rotated fault geometry and low friction along the faults appears to facilitate right lateral slip along the faults in western Alaska. Our results show that deformation well inside the continent can be explained in terms of the Pacific‐North American plate motions. Thus Tertiary plate motions have resulted in a broad zone of fault slip, uplift, and subsidence in the nonrigid North American plate, producing several large basins." @default.
• W2017030390 created "2016-06-24" @default.
• W2017030390 creator A5001581276 @default.
• W2017030390 creator A5034515345 @default.
• W2017030390 date "1990-12-01" @default.
• W2017030390 modified "2023-10-14" @default.
• W2017030390 title "Formation of interior basins associated with curved faults in Alaska" @default.
• W2017030390 cites W1038450508 @default.
• W2017030390 cites W1557211326 @default.
• W2017030390 cites W161936319 @default.
• W2017030390 cites W1966091017 @default.
• W2017030390 cites W1966717325 @default.
• W2017030390 cites W1966999633 @default.
• W2017030390 cites W1967824957 @default.
• W2017030390 cites W1967993402 @default.
• W2017030390 cites W1977156689 @default.
• W2017030390 cites W1981564263 @default.
• W2017030390 cites W1983202097 @default.
• W2017030390 cites W1984706377 @default.
• W2017030390 cites W1987135569 @default.
• W2017030390 cites W1988819584 @default.
• W2017030390 cites W1989698908 @default.
• W2017030390 cites W1990772221 @default.
• W2017030390 cites W1991886480 @default.
• W2017030390 cites W1995115331 @default.
• W2017030390 cites W1997041874 @default.
• W2017030390 cites W1999443818 @default.
• W2017030390 cites W2002133186 @default.
• W2017030390 cites W2002419284 @default.
• W2017030390 cites W2003174797 @default.
• W2017030390 cites W2004501456 @default.
• W2017030390 cites W2007788613 @default.
• W2017030390 cites W2008339911 @default.
• W2017030390 cites W2008695492 @default.
• W2017030390 cites W2009930154 @default.
• W2017030390 cites W2011452473 @default.
• W2017030390 cites W2012088192 @default.
• W2017030390 cites W2012422938 @default.
• W2017030390 cites W2013043947 @default.
• W2017030390 cites W2013548316 @default.
• W2017030390 cites W2014145087 @default.
• W2017030390 cites W2016307755 @default.
• W2017030390 cites W2016405844 @default.
• W2017030390 cites W2018618010 @default.
• W2017030390 cites W2020298416 @default.
• W2017030390 cites W2024953052 @default.
• W2017030390 cites W2027545308 @default.
• W2017030390 cites W2029743607 @default.
• W2017030390 cites W2031398064 @default.
• W2017030390 cites W2032764136 @default.
• W2017030390 cites W2034314180 @default.
• W2017030390 cites W2035360089 @default.
• W2017030390 cites W2035466761 @default.
• W2017030390 cites W2035860551 @default.
• W2017030390 cites W2036206765 @default.
• W2017030390 cites W2042911342 @default.
• W2017030390 cites W2043940160 @default.
• W2017030390 cites W2047516202 @default.
• W2017030390 cites W2048066852 @default.
• W2017030390 cites W2048624640 @default.
• W2017030390 cites W2049215404 @default.
• W2017030390 cites W2053692220 @default.
• W2017030390 cites W2057298949 @default.
• W2017030390 cites W2063172228 @default.
• W2017030390 cites W2064313622 @default.
• W2017030390 cites W2073875773 @default.
• W2017030390 cites W2074119724 @default.
• W2017030390 cites W2075598459 @default.
• W2017030390 cites W2075806947 @default.
• W2017030390 cites W2077989236 @default.
• W2017030390 cites W2078785429 @default.
• W2017030390 cites W2094586670 @default.
• W2017030390 cites W2096884377 @default.
• W2017030390 cites W2099718021 @default.
• W2017030390 cites W2103684543 @default.
• W2017030390 cites W2113929206 @default.
• W2017030390 cites W2115020762 @default.
• W2017030390 cites W2115931168 @default.
• W2017030390 cites W2117515460 @default.
• W2017030390 cites W2120691112 @default.
• W2017030390 cites W2126256158 @default.
• W2017030390 cites W2126652787 @default.
• W2017030390 cites W2129525615 @default.
• W2017030390 cites W2135494568 @default.
• W2017030390 cites W2150525715 @default.
• W2017030390 cites W2150666968 @default.
• W2017030390 cites W2157006453 @default.
• W2017030390 cites W2158923311 @default.
• W2017030390 cites W2160427602 @default.
• W2017030390 cites W2161699689 @default.
• W2017030390 cites W2483284175 @default.
• W2017030390 cites W3121831448 @default.
• W2017030390 cites W4239993598 @default.
• W2017030390 cites W4249413663 @default.
• W2017030390 cites W4293101087 @default.
• W2017030390 cites W64760061 @default.
• W2017030390 doi "https://doi.org/10.1029/tc009i006p01387" @default.
• W2017030390 hasPublicationYear "1990" @default.

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