FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2913946980> ?p ?o ?g. }

• W2913946980 endingPage "844" @default.
• W2913946980 startingPage "821" @default.
• W2913946980 abstract "We have analysed the geomorphic signatures in aggregation with the geomorphic indices with respect to hinterland and foreland neotectonic variability across the major Himalayan thrust system along the Kali River valley of eastern Kumaun Himalaya. The valley floor morphology in the vicinity of the major thrust gave rise to the accommodation space for the aggradation of the recent fluvial sediments. For a longitudinal distance of 212 km between the South Tibet Detachment (STD) and Himalayan Frontal Thrust (HFT), the valley has preserved significant aggradational landforms. These landforms have been physically examined to explain the spatial and temporal variability in phases of aggradation/incision in response to the tectonic activity during the late Quaternary. Fossil valleys and associated epigenetic gorges, cut‐and‐fill terraces with thick alluvial cover, debris‐flow terraces, bedrock strath terraces, and alluvial fan terraces are the significant aggradational landforms observed within the valley. They provide signatures of tectonic activity and past climatic records. We have analysed various geomorphic indices, namely, stream‐gradient index ( SL ), steepness index ( Ks ), hypsometric curve and index ( HI ), and asymmetric factor ( AF ) to map the spatial variability in tectonic processes across the major thrusts. The channel morphology (depth and width) of a river becomes adjusted in geological time because of long‐term tectonic and erosional processes. However, the channel geometry and deviations can be highly adjustable in a tectonically disturbed mountainous region. The deviations along the river course can be attributed to active tectonic movement along thrusts/faults or because of erosion/sedimentation processes. We applied a novel method called the river Gradient Length Anomaly (GLA) for 37 subbasins of the Kali River to deduce active deformation (uplift/subsidence) corresponding to the increased sedimentation and erosional rates, both from the upstream and downstream parts of the thrusted blocks, from where river flows through. The results of basin‐wise morphometric indices were corroborated with GLA anomaly and field observations, which suggests that the area has undergone active deformation between the Main Central Thrust (MCT) and Himalayan Frontal Thrust (HFT), which is attributed to the regional compression. The results of geomorphic and morphometric data are validated with the focal mechanisms of moderate earthquakes. The geomorphic analysis suggests that the hinterland part of eastern Kumaun is more active than the foreland region." @default.
• W2913946980 created "2019-02-21" @default.
• W2913946980 creator A5013139181 @default.
• W2913946980 creator A5026340789 @default.
• W2913946980 creator A5026646893 @default.
• W2913946980 date "2019-02-11" @default.
• W2913946980 modified "2023-10-16" @default.
• W2913946980 title "Evaluation of neotectonic variability along major Himalayan thrusts within the Kali River basin using geomorphic markers, Central Kumaun Himalaya, India" @default.
• W2913946980 cites W104554068 @default.
• W2913946980 cites W1442749281 @default.
• W2913946980 cites W1802706154 @default.
• W2913946980 cites W1824333283 @default.
• W2913946980 cites W1901082281 @default.
• W2913946980 cites W1964145151 @default.
• W2913946980 cites W1964639623 @default.
• W2913946980 cites W1965340864 @default.
• W2913946980 cites W1968107979 @default.
• W2913946980 cites W1969403464 @default.
• W2913946980 cites W1974184983 @default.
• W2913946980 cites W1976797497 @default.
• W2913946980 cites W1979877131 @default.
• W2913946980 cites W1983975910 @default.
• W2913946980 cites W1984314145 @default.
• W2913946980 cites W1986082054 @default.
• W2913946980 cites W1990519987 @default.
• W2913946980 cites W1993221937 @default.
• W2913946980 cites W1994516378 @default.
• W2913946980 cites W1994828817 @default.
• W2913946980 cites W1996164624 @default.
• W2913946980 cites W2000216327 @default.
• W2913946980 cites W2002325302 @default.
• W2913946980 cites W2003231782 @default.
• W2913946980 cites W2007831757 @default.
• W2913946980 cites W2010589603 @default.
• W2913946980 cites W2014650008 @default.
• W2913946980 cites W2019743413 @default.
• W2913946980 cites W2021393010 @default.
• W2913946980 cites W2022276037 @default.
• W2913946980 cites W2024423630 @default.
• W2913946980 cites W2024507466 @default.
• W2913946980 cites W2028140384 @default.
• W2913946980 cites W2029340380 @default.
• W2913946980 cites W2031599091 @default.
• W2913946980 cites W2036255205 @default.
• W2913946980 cites W2040110815 @default.
• W2913946980 cites W2040484660 @default.
• W2913946980 cites W2040820117 @default.
• W2913946980 cites W2044244301 @default.
• W2913946980 cites W2044723506 @default.
• W2913946980 cites W2046415826 @default.
• W2913946980 cites W2047424569 @default.
• W2913946980 cites W2047582516 @default.
• W2913946980 cites W2047661207 @default.
• W2913946980 cites W2051187614 @default.
• W2913946980 cites W2052421676 @default.
• W2913946980 cites W2056971404 @default.
• W2913946980 cites W2060198717 @default.
• W2913946980 cites W2064831569 @default.
• W2913946980 cites W2064972007 @default.
• W2913946980 cites W2066166725 @default.
• W2913946980 cites W2071237400 @default.
• W2913946980 cites W2071259160 @default.
• W2913946980 cites W2074307175 @default.
• W2913946980 cites W2075892097 @default.
• W2913946980 cites W2076062906 @default.
• W2913946980 cites W2076494384 @default.
• W2913946980 cites W2076665156 @default.
• W2913946980 cites W2080750700 @default.
• W2913946980 cites W2082300569 @default.
• W2913946980 cites W2090967889 @default.
• W2913946980 cites W2091319223 @default.
• W2913946980 cites W2093905602 @default.
• W2913946980 cites W2095134742 @default.
• W2913946980 cites W2096276260 @default.
• W2913946980 cites W2099265637 @default.
• W2913946980 cites W2101491699 @default.
• W2913946980 cites W2104300819 @default.
• W2913946980 cites W2106595832 @default.
• W2913946980 cites W2111204986 @default.
• W2913946980 cites W2117065525 @default.
• W2913946980 cites W2118381748 @default.
• W2913946980 cites W2120248779 @default.
• W2913946980 cites W2120764192 @default.
• W2913946980 cites W2122195782 @default.
• W2913946980 cites W2125217075 @default.
• W2913946980 cites W2126323973 @default.
• W2913946980 cites W2127128063 @default.
• W2913946980 cites W2127220873 @default.
• W2913946980 cites W2134418689 @default.
• W2913946980 cites W2138724462 @default.
• W2913946980 cites W2144583290 @default.
• W2913946980 cites W2145791900 @default.
• W2913946980 cites W2149929044 @default.
• W2913946980 cites W2155880045 @default.
• W2913946980 cites W2159569412 @default.
• W2913946980 cites W2224254779 @default.
• W2913946980 cites W2292700980 @default.
• W2913946980 cites W2312463568 @default.

• next