N. Suresh, S. K. Ghosh, R. Kumar and S. J. Sangode, “Clay Mineral Distribution Pattern in Late Neogene Fluvial Sediments of Subathu Sub-Basin, Central Sector of Himalayan Foreland Basin: Implication for Provenance and Climatic Condition,” Sedimentary Geology, Vol. 163, No. 3-4, 2004, pp. 265-278.
http://dx.doi.org/10.1016/j.sedgeo.2003.07.006

has been cited by the following article:

• TITLE: Size Analysis of the Late Pliocene-Early Pleistocene Upper Siwalik Sediments, Northwestern Himalaya, India

  AUTHORS: Mahavir Singh, A. R. Chaudhri

  KEYWORDS: Texture; Siwalik; Pinjor; Himalaya

  JOURNAL NAME: International Journal of Geosciences, Vol.4 No.8, October 15, 2013

  ABSTRACT: Size analysis of the Late Pliocene-Early Pleistocene Upper Siwalik sediments comprising the Pinjor Formation in the type area and adjoining regions reveals that the sediments are bimodal to polymodal in nature, medium to fine grained and are moderately sorted. The inclusive graphic standard deviation and moment standard deviation values suggest the deposition of sediments in shallow to moderately deep fluvial agitated water. The log probability plots reveal that saltation mode is the dominant mode of transportation of detritus. The sediments are continental in character and are derived from crystalline, metamorphic and sedimentary rocks of the Himalaya exposed to the North of the type area Pinjor.