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In the part of Sikkimese-Bhutanese Himalaya the youngest Siwalik overthrust had not developed, and the piedmont zone with extensive fans forms a semicircular gulf dismembered by several faults and minor overthrusts. Some uplifted parts of older deformed alluvial fans contain the lenses of organic clays which were earlier dated at 22–34 ka BP by 14C method. Various elevated levels differ also in soil maturity. It means that the main tectonic activity with overthrusting could occur later. To distinguish various alluvial formations and phases of tectonic activity the authors dated older levels in several localities by OSL method as well as investigated soil profiles. Most mature soils over elevated blocks built of coarse alluvia were dated between 50 and 60 ka BP. Probably the previous 14C dates from clays are too young, and on the contrary OSL dates are overestimated. The younger generation of fans (10–15 m high) dated at about 14 ka coincide with the start of monsoonal pre-Holocene activity. The authors try to correlate these phases with terraces and tectonic activity in the most eastern part of the Himalayas (two phases of overthrusting: after 50 ka and 10–5 ka BP) as well as with events outside the piedmont zone: glacifluvial aggradation in the Tista valley during advance of glaciers in Sikkim and with sequence of deposits in the Brahmaputra delta.
Wydawca
Czasopismo
Rocznik
Tom
Strony
71--82
Opis fizyczny
Bibliogr. 21 poz., rys.
Twórcy
autor
- Institute of Geography and Spatial Organization PAS, Department of Geoenvironmental Research; 22 Św. Jana str., 31-018 Krakow, Poland
autor
- Institute of Geography and Spatial Organization PAS, Department of Geoenvironmental Research; 22 Św. Jana str., 31-018 Krakow, Poland
autor
- Silesian University of Technology, Institute of Physics; 2 Krzywoustego str., 44-100 Gliwice, Poland
Bibliografia
- Abrahami R., Huyghe P., van der Beck P., Carcaillet J., Chakraborty T., 2013. The detrital thermochronologic and cosmogenic data to understand the evolution of modern Himalayan megafans. [in:] Int. Conference of IAG, Paris Abstracts of papers 505, p. 219.
- Adamiec G., Aitken M.J, 1998. Dose-rate conversion factors: update. Ancient TL 16(2), 37–50.
- Basu S.R., Sarkar S., 1990. Development of alluvial fans in the foot-hills of the Darjeeling Himalayas and their geomorphological and pedological characteristics. [in:] Alluvial Fans: a Field Approach. A.H. Rachocki, M. Church (eds.), J. Wiley, Chichester, 321–333.
- Bluszcz A., Starkel L., Kalicki T., 1997. Grain size composition and age ofalluvial sediments in Tista valley floor near Kalijhora, Sikkim Himalaya. Studia Geomorphologica Carpatho-Balcanica 31, 159–174.
- Bortolot V.J., 2000. A new modular high capacity OSL reader system. Radiation Measurements 32, 751–757.
- Das A., Chattopadhyay G.S., 1993a. Neotectonics in Tista – Jaldhaka and Torsa interfluves belt of north Bengal. Geological Survey of India Records 121, 2–8, 101–109.
- Das A., Chattopadhyay G.S., 1993b. Use of soil in building up the Quaternary stratigraphy of north Bengal. Geological Survey of India Records, 121, 2–9, 87–91.
- Gansser A., 1964. Geology of Himalayas. Interscience, New York, 289 pp.
- Guha D., Bardhan S., Basir S.R., De A.K., Sarkar A., 2007. Imprints of Himalayan thrust tectonics on the Quaternary piedmont sediments of the Neora-Jaldhaka Valley, Darjeeling-Sikkim sub-Himalayas, India, Journal of Asian Earth Sciences 30, 464–473.
- Kale V.S., Gupta A., Singhvi A.K., 2003. Late Pleistocene-Holocene paleohydrology of monsoon Asia. [in:] Paleohydrology, Understanding Global Change. K.J. Gregory, G. Benito, (eds.), J. Wiley, Chichester, 213–232.
- Luirei K., Bhakuni S.S., Srivastava P., Suresh N., 2012. Late Pleistocene – Holocene tectonic activities in the frontal part of NE Himalaya between Siang and Dibang river valleys, Arunachal Pradesh, India. Zeitschrift für Geomorphologie 56, 4, 477–493.
- Murray A.S., Wintle A. G., 2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32, 57–73.
- Nakata T., 1972. Geomorphic history and crustal movements of the foot-hills of the Himalayas. The Scientific Reports of the Tohoku University, VII Series, Geography 22, 1, Sendai, 39–177.
- Nakata T., 1989. Active faults of the Himalaya of India and Nepal. Geological Society of America, Special Paper, 232, 243–264.
- Overpeck J., Anderson D., Trambore S., P rell W., 1996. The southwest Indian monsoon over the last 18000 years. Climate Dynamics 12, 213–225.
- Prescott J.R., Hutton J.T., 1994. Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations. Radiation Measurements 23, 497–500.
- Srivastava P., Bhakuni S.S., Luirei K., Misra D.K., 2009. Morphosedimentary records at the Brahmaputra River exit, NE Himalaya: climate-tectonic interplay during Late Pleistocene-Holocene. Journal of Quaternary Science 24, 175–188.
- Starkel L., Basu S., (eds.), 2000. Rains, Landslides and Floods in the Darjeeling Himalaya. INSA, New Delhi, 168 pp.
- Starkel L., Sarkar S., Soja R., P rokop P., 2008. Present-day evolution of the Sikkimese-Bhutanese Himalayan piedmont. Prace Geograficzne IGiPZ PAN 219, 7–178.
- Umitsu M., 1987. Late Quaternary sedimentary environment and landform evolution in the Bengal Lowland. Geographical Review of Japan (Series B), 60, 164–178.
- Valdiya K.S., 1998. Dynamic Himalaya, Educational Monographs. University Press, India, 178 pp.
Typ dokumentu
Bibliografia
Identyfikator YADDA
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