Age of the Baula PGE mineralization (Orissa, India) and its implications concerning the Singhbhum Archaean nucleus

[1]  K. Ludwig User's Manual for Isoplot 3.00 - A Geochronological Toolkit for Microsoft Excel , 2003 .

[2]  L. Bailly,et al.  MAGMATIC AND HYDROTHERMAL PLATINUM-GROUP MINERALS AND BASE-METAL SULFIDES IN THE BAULA COMPLEX, INDIA , 2002 .

[3]  M. Glascock,et al.  PGE AND Ag MINERALIZATION IN A BRECCIA ZONE OF THE PRECAMBRIAN NUASAHI ULTRAMAFIC-MAFIC COMPLEX, ORISSA, INDIA , 2001 .

[4]  D. Mukhopadhyay The Archaean nucleus of Singhbhum: the present state of knowledge , 2001 .

[5]  A. R. Butcher,et al.  Platinum-group mineralization in the Tertiary Igneous Province: new data from Mull and Skye, Scottish Inner Hebrides, UK , 2000, Geological Magazine.

[6]  P. Mathur,et al.  PGE-Ag-Au Mineralization in a Cu-Fe-Ni Sulphide-Rich Breccia Zone of the Precambrian Nuasahi Ultramafic-Mafic Complex, Orissa, India , 1999 .

[7]  A. Saha,et al.  207Pb/206Pb zircon ages and the evolution of the Singhbhum Craton, eastern India: an ion microprobe study , 1999 .

[8]  J. Kramers,et al.  Nd isotopic evolution of the upper mantle during the Precambrian: models, data and the uncertainty of both , 1998 .

[9]  S. Mondal,et al.  Platinum-Group Minerals from the Nuasahi Ultramafic-Mafic Complex, Orissa, India , 1997 .

[10]  B. Chadwick Crustal evolution of singhbhum-North Orissa, Eastern India: A.K. Saha. Memoir 27, Geological Society of India, Bangalore, 1994, Paperback, xii + 341 pp., US$30.-, ISBN 81-85867-09-7 , 1996 .

[11]  W. McClelland,et al.  U-Pb reverse discordance in zircons: The role of fine-scale oscillatory zoning and sub-micron transport of Pb , 1996 .

[12]  A. Basu,et al.  Sm-Nd Isotopic and Geochemical Study of the Archean Tonalite-Amphibolite association from the eastern Indian Craton , 1994 .

[13]  J. D. Miller,et al.  Precise U‐Pb ages of Duluth Complex and related mafic intrusions, northeastern Minnesota: Geochronological insights to physical, petrogenetic, paleomagnetic, and tectonomagmatic processes associated with the 1.1 Ga Midcontinent Rift System , 1993 .

[14]  D. Hoatson,et al.  Distribution of sulphides and PGE within the porphyritic websterite zone of the Munni Munni Complex, Western Australia , 1992 .

[15]  A. M. Thorne,et al.  The age of the Fortescue Group, Hamersley Basin, Western Australia, from ion microprobe zircon U-Pb results , 1991 .

[16]  D. Paul,et al.  Rb-Sr age of granitoid in the Deo River Section, Singhbhum and its relevance to the age of iron formation , 1991 .

[17]  R. J. Hart,et al.  Platinum group elements in a 3.5 Ga nickel‐iron occurrence: Possible evidence of a deep mantle origin , 1989 .

[18]  N. J. Page,et al.  Characterization of the Sukinda and Nausahi ultramafic complexes, Orissa, India by platinum-group element geochemistry , 1985 .

[19]  W. Compston,et al.  Unsupported radiogenic Pb in zircon: a cause of anomalously high Pb-Pb, U-Pb and Th-Pb ages , 1984 .

[20]  A. Saha,et al.  The structural and geochemical evolution of the Singhbhum granite batholithic complex, India , 1984 .

[21]  N. Shimizu,et al.  143Nd/146Nd, a natural tracer: an application to oceanic basalts* , 1976 .