Palaeoproterozoic fluvio-aeolian deposits from the lower Gulcheru Formation, Cuddapah Basin, India

[1]  V. Packard Imperial Gazetteer of India , 2013 .

[2]  E. Simpson,et al.  3.2Ga eolian deposits from the Moodies Group, Barberton Greenstone Belt, South Africa: Implications for the origin of first-cycle quartz sandstones , 2012 .

[3]  P. Dasgupta,et al.  Geometrical mechanism of inverse grading in grain-flow deposits: An experimental revelation , 2011 .

[4]  Jennifer N. Gifford,et al.  Precambrian crustal evolution of Peninsular India: A 3.0 billion year odyssey , 2010 .

[5]  Himadri Basu,et al.  Study of provenance characteristics and depositional history on the basis of U, Th and K abundances in the Gulcheru Formation, Cuddapah Basin in Tummalapalle-Somalollapalle areas, Cuddapah-Anantapur Districts, Andhra Pradesh , 2009 .

[6]  T. Kano,et al.  Petrology and geochemistry of late archaean granitoids in the northern part of Eastern Dharwar Craton, Southern India: Implications for transitional geodynamic setting , 2009 .

[7]  T. Chakraborty,et al.  Shallow marine and coastal eolian quartz arenites in the Neoarchean-Palaeoproterozoic Karutola Formation, Dongargarh Volcano-sedimentary succession, central India , 2008 .

[8]  R. Srivastava,et al.  1891–1883 Ma Southern Bastar–Cuddapah mafic igneous events, India: A newly recognized large igneous province , 2008 .

[9]  O. Pandey,et al.  Imprints of a Proterozoic tectonothermal anomaly below the 1.1 Ga kimberlitic province of Southwest Cuddapah basin, Dharwar craton (Southern India) , 2008 .

[10]  O. Catuneanu,et al.  Prime controls on Archaean–Palaeoproterozoic sedimentation: Change over time , 2007 .

[11]  H. Basu Geological and Geochemical Aspects of the Gulcheru Formation in the Southwestern Margin of the Cuddapah Basin and its Potentiality for Uranium Mineralisation , 2007 .

[12]  Michael A. Hamilton,et al.  Paleomagnetism and U-Pb geochronology of easterly trending dykes in the Dharwar craton, India: feldspar clouding, radiating dyke swarms and the position of India at 2.37 Ga , 2007 .

[13]  Suresh Kuman,et al.  Sedimentary Facies of Gulcheru Quartzite in the Southwestern Part of the Cuddapah Basin and their Implication in Deciphering the Depositional Environment , 2007 .

[14]  P. Dasgupta Facies characteristics of Talchir Formation, Jharia Basin, India: Implications for initiation of Gondwana sedimentation , 2006 .

[15]  A. Biswas Coarse aeolianites: sand sheets and zibar–interzibar facies from the Mesoproterozoic Cuddapah Basin, India , 2005 .

[16]  E. Simpson,et al.  Saline pan deposits from the ∼1.8 Ga Makgabeng Formation, Waterberg Group, South Africa , 2004 .

[17]  S. Kelley,et al.  Early Proterozoic Melt Generation Processes beneath the Intra-cratonic Cuddapah Basin, Southern India , 2003 .

[18]  J. Moyen,et al.  Late Archaean granites: a typology based on the Dharwar Craton (India) , 2003 .

[19]  P. Dasgupta Sediment gravity flow—the conceptual problems , 2003 .

[20]  J. D. H. Dott The Importance of Eolian Abrasion in Supermature Quartz Sandstones and the Paradox of Weathering on Vegetation‐Free Landscapes , 2003 .

[21]  D. C. Mishra,et al.  Tectonosedimentary evolution of Cuddapah basin and Eastern Ghats mobile belt (India) as Proterozoic collision: gravity, seismic and geodynamic constraints , 2002 .

[22]  E. Simpson,et al.  Eolian Dune Degradation and Generation of Massive Sandstone Bodies in the Paleoproterozoic Makgabeng Formation, Waterberg Group, South Africa , 2002 .

[23]  G. Ghosh,et al.  The Purana Basins of Southern Cratonic Province of India - A Case for Mesoproterozoic Fossil Rifts , 2002 .

[24]  N. Chatterjee,et al.  Petrology, geochemistry and tectonic settings of the mafic dikes and sills associated with the evolution of the Proterozoic Cuddapah Basin of south India , 2001 .

[25]  S. V. Srikantia Geological Map of India , 2001 .

[26]  G. Hegde,et al.  The Dharwar craton, southern India, interpreted as the result of Late Archaean oblique convergence , 2000 .

[27]  G. Nichols Sedimentology and Stratigraphy , 1999 .

[28]  Y. Sohn,et al.  Debris Flow and Hyperconcentrated Flood‐Flow Deposits in an Alluvial Fan, Northwestern Part of the Cretaceous Yongdong Basin, Central Korea , 1999, The Journal of Geology.

[29]  S. Sarkar,et al.  Recognition of ancient eolian longitudinal dunes; a case study in upper Bhander Sandstone, Son Valley, India , 1999 .

[30]  E. Simpson,et al.  Controls on spatial and temporal distribution of Precambrian eolianites , 1998 .

[31]  J. Chiarenzelli,et al.  Initiation of ̃2.45-2.1 Ga intracratonic basin sedimentation of the Hurwitz Group, Keewatin Hinterland, Northwest territories, Canada , 1997 .

[32]  G. Shanmugam High-Density Turbidity Currents: Are They Sandy Debris Flows?: PERSPECTIVES , 1996 .

[33]  V. S. Kale,et al.  An Unusual Evaporite Association from the Papaghni Group, Cuddapah Basin , 1992 .

[34]  V. S. Kale Constraints on the Evolution of the Purana Basins of Peninsular India , 1991 .

[35]  T. Chakraborty Sedimentology of a Proterozoic erg: the Venkatpur Sandstone, Pranhita-Godavari Valley, south India , 1991 .

[36]  C. Snyman,et al.  The sedimentology of the Waterberg Group in the Transvaal, South Africa: an overview , 1991 .

[37]  Gary A. Smith,et al.  Lahars : volcano-hydrologic events and deposition in the debris flow-hyperconcentrated flow continuum. , 1991 .

[38]  C. X. R. K. Prasad,et al.  Quartzites of the Cuddapah Group and Their Environment of Deposition , 1990 .

[39]  R. Langford,et al.  Fluvial-aeolian interactions: Part II, ancient systems , 1989 .

[40]  C. J. Schenk,et al.  Pin stripe lamination: A distinctive feature of modern and ancient eolian sediments , 1988 .

[41]  B. R. Babu,et al.  Stratigraphy, structure, and evolution of the Cuddapah Basin , 1987 .

[42]  R. Venkatakrishnan,et al.  The Cuddapah Salient: a tectonic model for the Cuddapah Basin, India, based on Landsat image interpretation , 1987 .

[43]  G. Kocurek,et al.  Conditions favourable for the formation of warm-climate aeolian sand sheets , 1986 .

[44]  R. Kostaschuk,et al.  Depositional process and alluvial fan‐drainage basin morphometric relationships near banff, Alberta, Canada , 1986 .

[45]  R. Dott,et al.  Aeolian to marine transition in Cambro—Ordovician cratonic sheet sandstones of the northern Mississippi valley, U.S.A. , 1986 .

[46]  Gary A. Smith Coarse-grained nonmarine volcaniclastic sediment : terminology and depositional process , 1986 .

[47]  W. Nemec,et al.  Alluvial and Coastal Conglomerates: Their Significant Features and Some Comments on Gravelly Mass-Flow Deposits , 1984 .

[48]  A. Basu,et al.  Climate and the origin of quartz arenites , 1981 .

[49]  G. Kocurek,et al.  Distinctions and Uses of Stratification Types in the Interpretation of Eolian Sand , 1981 .

[50]  Thomas S. Ahlbrandt,et al.  Origin, sedimentary features, and significance of low-angle eolian "sand sheet" deposits, Great Sand Dunes National Monument and vicinity, Colorado , 1979 .

[51]  K. Kaila,et al.  Crustal Structure Along Kavali-Udipi Profile in the Indian Peninsular Shield from Deep Seismic Sounding , 1979 .

[52]  R. E. Hunter Basic types of stratification in small eolian dunes , 1977 .

[53]  I. E. Odom Feldspar-grain size relations in Cambrian arenites, upper Mississippi Valley , 1975 .

[54]  H. Reineck,et al.  Depositional sedimentary environments , 1973 .

[55]  Raymond Siever,et al.  Sand and sandstone , 1972 .