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The AAPG/Datapages Combined Publications Database

Montana Geological Society

Abstract

MTGS-AAPG

Montana Geological Society and Yellowstone Bighorn Research Association Joint Field Conference and Symposium: Geology of the Beartooth Uplift and Adjacent Basins
---, 1986

Pages 155 - 164

SOME FEATURES INDICATING TECTONIC DENUDATION BY THE HEART MOUNTAIN Previous HitFAULTNext Hit

William G. Pierce, U.S Geological Survey, Menlo Park, California 94025
Willis H. Nelson, U.S Geological Survey, Menlo Park, California 94025

ABSTRACT

Two basic concepts pertaining to the Heart Mountain Previous HitfaultNext Hit have recently been challenged (Hauge, 1982a, 1982b, 1982c, 1983a, 1983b, 1985); one, that there was tectonic denudation, and two, that volcanic rock of the Wapiti Formation was deposited on the exposed Previous HitfaultNext Hit surface. We believe that tectonic denudation occurred as a consequence of the upper plate having broken up into numerous blocks that separated as movement progressed along a nearly horizontal Previous HitfaultNext Hit surface, thus leaving the Previous HitfaultNext Hit surface exposed between blocks. Volcanic rocks of the Wapiti Formation were then deposited on the exposed Previous HitfaultNext Hit surface. Documentation of the validity of this concept depends in part upon recognizing two formations of Eocene volcanic rocks. The older Cathedral Cliffs Formation, together with Paleozoic carbonate rocks, is part of the upper plate of the Heart Mountain Previous HitfaultNext Hit and moved with it, whereas the younger Wapiti Formation was deposited on the Previous HitfaultNext Hit surface after movement had ceased.

In the alternate interpretation recently advanced, subdivisions of the Absaroka Volcanic Supergroup, of which the Cathedral Cliffs and Wapiti Formations are units, are not recognized and it is concluded that, "During Heart Mountain faulting, extension of the once-continuous slab of Palezoic sedimentary rock was accompanied by the formation of ten or more graben now composed dominantly of Absaroka volcanic rocks" (Hauge, 1982b, p. 178). This interpretation further proposed that the volcanic rock infilling took place while the separating blocks of Palezoic strata were still moving and that the basal part of the volcanic rock between these blocks is in Previous HitfaultNext Hit contact rather than depositional contact with the strata beneath the Heart Mountain Previous HitfaultNext Hit. More recently, Hauge (1985) has suggested a gravity-spreading origin of the Heart Mountain allochthon, in which the mechanism of emplacement of the allochthon, which once may have covered more than 3,400 km2, is viewed in terms of gravity-induced spreading on the flanks of an active volcanic field.

Geologic evidence that supports our contention that the Wapiti Formation is younger than the Heart Mountain Previous HitfaultNext Hit and was not Previous HitfaultNext Hit-emplaced include: (1) A break-away Previous HitfaultNext Hit cuts the Paleozoic carbonate rocks and Cathedral Cliffs Formation, but is overlain by several thousand feet of unbroken Wapiti Formation; (2) The volume of Wapiti Formation filling the spaces between allochthon blocks is much too great to have been allochthonous as part of the upper plate; (3) The Previous HitfaultNext Hit breccia at the base of the upper plate carbonate blocks is composed entirely of carbonate Previous HitfaultNext Hit breccia, with no volcanic contribution; (4) small blocks have been transported from the upper part of the allochthon to the Previous HitfaultNext Hit surface; (5) Wapiti volcanic rocks with chilled borders are in tightly bonded or "frozen" contact with upper plate Paleozoic rocks; (6) Faults present in the upper plate blocks do not enter the overlying Wapiti Formation; and (7) absence of volcanic Previous HitfaultNext Hit breccia where volcanic rocks overlie carbonate Previous HitfaultTop breccia.

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