Glenn t. thong's 5 research works with 42 citations and 1,962 reads, including: late quaternary deformation in parts of the belt of schuppen of dimapur and peren districts, nagaland, ne india. May 6, 2011 the naga thrust belt is a narrow, elongated zone of imbricate thrusts about 20 to 35 km wide, extending for about 200 km in a ne-. sw direction. The schuppen belt covers the western margin of nagaland state for about 200 kilometer trending ne-sw. the 20 to 30 km wide exposed part of schuppen belt comprises two major thrusts (haflong-naga thrust, disang thrust) and three minor schuppen belt sub-thrusts.
Haflong Thrust Wikipedia
Jan 5, 2014 the schuppen belt of north-east india forms the outermost fringe of the mobile belt of the assam–arakan basin (ranga rao and samanta, 1987). Request pdf on aug 9, 2013, tanaya ghosh and others published geological mapping of the schuppen belt of north-east india using geospatial technology .
The schuppen belt of north-east india forms the outermost fringe of the mobile belt of the assam–arakan basin. this ne–sw trending belt is bounded by naga thrust in the north-west and disang thrust in the south–east. it extends from schuppen belt maibong (assam. Jan 8, 2019 geomorphic evidences and geochronology suggest recent tectonic activity in the belt of schuppen of dimapur and peren districts of nagaland.
Haflong Thrust Wikipedia
The southern part of 'belt of schuppen' extends along the sheared western limb of southerly plunging kohima synform, a part of indo burma ranges (ibr) and it is seismically active. schuppen belt the crustal velocity at se of schuppen is 39. 90 mm/yr with a azimuth of 70. 780 at lumami, 38. 84 mm/yr (azimuth 54. 09) at senapati and 36. 85 mm/yr (azimuth 54. 09) at. Mar 31, 2019 the belt of schuppen is an important tectonic element of the assam-arakan basin. it is a narrow belt of thrust slices in southeastern boundary of . The naga schuppen belt, a zone of imbricate thrusting involving the paleogene-neogene foreland sediments (mathur et al. 2001), occurs between the naga and disang thrusts; the shelf-to-basinal slope transition hinge zone probably lies beneath the naga schuppen belt whereas the basinal sediments are seen in the assam-arakan and the chittagong. Mar 31, 2019 the belt of schuppen is an important tectonic element of the assam-arakan basin. it is a narrow belt of thrust slices in southeastern boundary of .
Using aerial photographs followed by extensive field checks, a photo-geological map for the entire 'belt of schuppen' of northeast india has been prepared. Examples of schuppen described from other regions of folding and associated utah: structure of the provo salient's northern margin, sevier fold–thrust belt.
Glenn t. thong's research works nagaland university.
Haflong thrust wikipedia.
Dec 13, 2015 the schuppen belt of north-east india forms the outermost fringe of the mobile belt of the assam–arakan basin. this ne–sw trending belt is . This type of imbricate thrust system has been described by suess (1904) as ' schuppen belt'. the belt of schuppen (bos) in nagaland is delineated on the east by . The schuppen belt of north-east india forms the outermost fringe of the mobile belt of the assam–arakan basin (ranga rao and samanta, 1987). this ne–sw trending belt is bounded by naga thrust in the north-west and disang thrust in the south–east (evans, 1964). it extends from maibong (assam) in south to mishmi hills (arunachal pradesh) in north. Naga-schuppen belt. some of these sequences hold hydrocarbon pools in the northern part of the belt. therefore, this inadequately explored prospective belt is of great interest for finding good sized schuppen belt pools in the south-western part of belt in fault controlled traps. methodology and results. in this present study, post drill pore pressure analysis.
The haflong thrust is the most persistent of the thrusts in the 400 km long belt of schuppen (bos) in the western part of nagaland. the belt of schuppen forms . A revised geologic map of the schuppen belt of northeast india has been prepared based on interpretation of digitally enhanced satellite images. the satellite image interpretation is supported by limited field work and existing geologic maps. available geological maps of this fold thrust belt are discontinuous and multi-scaled. the authors are of multiple opinions regarding the trajectory of. The naga schuppen zone,occurring between the naga and the disang thrusts. in this shelf–slope–basinal architecture, the hinge zone, at and across which the upper cretaceous-eocene shelf facies changes over to basinal facies, is envisaged to lie below the naga schuppen belt. the kharsang, digboi and champang oil fields are located in this. While studying the structure and tectonics of north-east india, schuppen belt finds an important place. it is an imbricately faulted / thrusted belt of cenozoic .
This type of imbricate thrust system has been described by suess (1904) as 'schuppen belt'. the belt of schuppen (bos) in nagaland is delineated on the east by . Geomorphic evidences and geochronology suggest recent tectonic activity in the belt of schuppen of dimapur and peren districts of nagaland. multiple levels of strath ter-races forming remarkable geomorphic expressions schuppen belt are observed along the chathe and jharnapani river valleys. they indicate episodic uplift of the hanging‐wall blocks of the.
