Chronology of red dune aggradations of South India and its Palaeo-environmental significance

• Autorzy: Alappat L. , Seralathan P. , Shukla A. D. , Thrivikramji K. P. , Singhvi A. K.
• Języki publikacji: EN

Abstrakty

EN

Red sand dunes occur in the coastal plains of south east and west of Tamil Nadu, India be-tween the co-ordinates of 8°00’ to 9°30’ N; 77°18’ to 79° 00’ E. OSL dating of these sands indicated aggradations between ~16-9 ka and ~9-3 ka in the west and east coasts respectively. Dating results from inland red dunes at the foothills of Western Ghats show a break in deposition at ~6 ka and ag-gradation since ~2 ka. The sand aggradations in the west coast occurred during the transition period when SW monsoon in the area was re-establishing. The dunes attained their stability by 9 ka. In the coastal region, the aggradations were controlled by sea level changes and a local recycling of earlier dunes (in the east coast). In the inland areas, the dune building was controlled by sand supply from fluvial sources.

Słowa kluczowe

EN

red sand dunes; OSL dating; Pleistocene; Holocene; chronology; sand aggradations

• Wydawca: De Gruyter
• Czasopismo: Geochronometria
• Rocznik: 2013
• Tom: Vol. 40, no. 4
• Strony: 274--282
• Opis fizyczny: Bibliogr. 45 poz., tab., wykr.

Twórcy

autor

Alappat L.

• Geosciences Division, Physical Research Laboratory, Ahmedabad, India

autor

Seralathan P.

• Department of Marine Geology and Geophysics, Cochin University of Science and Technology, Kerala, India

autor

Shukla A. D.

• Geosciences Division, Physical Research Laboratory, Ahmedabad, India

autor

Thrivikramji K. P.

• UGC Emeritus Fellow, Dept. of Geology, University of Kerala, Kariavattom Campus, Trivandrum, India

autor

Singhvi A. K.

• Geosciences Division, Physical Research Laboratory, Ahmedabad, India

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