Geochemical clues to elucidate the tectonic environment of the Chamoli Volcanics, Lesser Himalayas, Uttar Pradesh, India

Geochemical data on the Chamoli Volcanics of the Garhwal Group suggest their strong affinity with oceanic tholeiites. However, the field relations and other geological information do not support this conclusion and indicate an epicontinental rather than eugeosynclinal environment of eruption. The lack of correlation of chemical data with geological setting precludes the possibility that these basalts are true ocean floor basalts. It is inferred that the Chamoli Volcanics with an oceanic tholeiite affinity were probably erupted as a result of initial rifting in the Proto-Tethys, which at that time was an intercontinental sea. The rifting was started during the depositional regimes of this intercontinental sea in which shallow water sediments were being deposited. Ocean type tholeiitic magma, guided by the rift zone, disrupted the cycle of sedimentation and gave rise to the development of the quartzite-lava sequence of the Chamoli Formation.