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Title: Precambrian geology and bedded iron deposits of the southwestern Ruby Range, Montana

Journal Article · · United States Geological Survey, Professional Paper; (USA)
OSTI ID:6317498

The Precambrian crystalline rocks of the southwestern Ruby Range, an area of about 100 square miles, can be divided roughly into three northeast-trending belts, progressively younger to the west.The oldest and most easterly belt consists of an ill-defined sequence of Early( ) or Middle( ) Archean older gneiss and schist that underlies, with structural conformity, a central belt underlain in turn by a rudely tabular mass of Middle or late Archean quartzofeldspathic gneiss that forms the crest of the range for much of its length. This quartzofeldspathic gneiss forms a basement complex to an overlying sequence of metasedimentary strata that make up the most westerly of the three belts. The Middle or Late Archean metasedimentary sequence, here named the Christensen Ranch Metasedimentary Suite, consisted originally of miogeoclinal-type sedimentary rocks, now represented by dolomite marble, diopsidic and hornblendic gneiss and schist, quartzite, mica and garnet schist, and banded iron-formation. Amphibolite of Middle or Late Archean age is an abundant rock type, occurring as generally conformable screens and sheets, some as much as several thousand feet in thickness, in each of the three main rock groups. Known or potential mineral resources include talc, graphite, and banded iron-formation. The iron-formation has been explored extensively in the Carter Creek area; these deposits are estimated to contain about 95 million tons of rock containing 28-29% iron recoverable as magnetite. The Kelly iron deposit is in the northeastern part of the Ruby Range. The iron-formation in this upthrust block has been explored by test pits and drill holes, but despite a favorable composition, the economic potential is low; deposits are estimated to be about 15 million tons containing 33% iron recoverable as magnetite.

OSTI ID:
6317498
Journal Information:
United States Geological Survey, Professional Paper; (USA), Vol. 1495
Country of Publication:
United States
Language:
English