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K. Pye, “Late Quaternary Development of Coastal Parabolic Megadune Complexes In Northeastern Australia, in Eolian Sediments: Ancient and Modern,” In: K. Pye and N. Lancaster, Eds., International Association of Sedimentology, Blackwell Science, Oxford, Special Publishing, Vol. 16, 1993, pp. 23-44.

has been cited by the following article:

• TITLE: Interpretation of Dune Genesis from Sedimentogical Data and Ground Penetrating Radar (GPR) Signatures: A Case Study from Ashirmata Dune Field, Mandvi Beach, Gujarat, India

  AUTHORS: Deshraj Trivedi, Koravangatt Devi, Ilya Buynevich, P. Srinivasan, K. Ravisankar, Vipul Silwal, D. Sengupta, Rajesh R. Nair

  KEYWORDS: Coastal Dune; Ashirmata Region; Sedimentogical Analysis; Ground Penetrating Radar; Paleosol

  JOURNAL NAME: International Journal of Geosciences, Vol.3 No.4, September 11, 2012

  ABSTRACT: The coastal dunes located near the Ashirmata region, south of Mandvi beach lies near the straight coast have been stud-ied by making use of sedimentological information and Ground Penetrating Radar (GPR) data. Sedimentological analy-sis reveals the NNW-SSE trending longitudinal dunes consists of well sorted fine sands with unimodal distribution pos-sibly formed by constant wind gust and also the point out to the origin of sediments from single source; mostly the sediments derived from Indus delta transported to beach by long shore drift and tidal waves, carried inland by local on-shore winds. The radargram confirms, the homogenous sand layers with paleosols at shallow depth slip faces are proba-bly formed due to extreme storm activity of Recent.