Sixty nine(69) samples of Deccan basalt flows from the Western Ghats r
epresenting the Wai, Lonavala,and Kalsubai subgroups average 3.7 ppb o
f gold. Gold content shows limited variation from 3.0 to 5.8 ppb in 62
samples whereas they range from 1.4 to 2.7 ppb in 7 samples. Flows of
the Wai subgroup show the maximum variation in gold abundances (1.4 -
5.8 ppb) and which may be related to the presence of primitive. uncon
taminated basalts (Anibenali)- lowest value.-crust-contaminated basalt
s (Poladpur) and ba.-alls derived from enriched-mantle sources (Mahaba
leshwar). Gold appears to be insensitive to crystal fractionation or d
ifferentiation as basalts of different types such as the picritic, por
phyritic, aphyric and giant plagioclase-bearing types found within a s
ubgroup or formation have similar averages (3.6 - 3.8 ppb). Deccan tho
leiitic basalts contain higher amounts of gold than some of the ocean
island (Hawaii) tholeiitic basalts, island arc (Kurile-Kamchatka) thol
eiites, but contain values similar to those found in the Columbia Rive
r basalt province.