A. Basu et al., PETROLOGY AND GEOCHEMISTRY OF THE LAMPROPHYRIC ROCKS FROM THE BOKARO COALFIELD, BIHAR AND THEIR ECONOMIC-POTENTIAL, Journal of the Geological Society of India, 50(3), 1997, pp. 255-266
The dyke swarms intruding the Gondwana sequence in the east Bokaro Coa
lfrield, Bihar include lamprophyres and lamproites such as olivine lam
proties, olivine-leucite lamproites and leucite lamproites. Basic intr
usives and rare siderite rich carbonates (carbonatite ?) are also foun
d. The olivine lamproites contain xenocrysts of olivine and rare xenol
iths of harzburgite. Gold Values upto 3.6 ppm on grab samples have bee
n noted from the intrusive rocks in the area. These lamprophyric rocks
are considered to have formed from a highly incompatible element enri
ched metasomatised mantle source probably of harzburgitic composition.