The
Book
Canyon Conglomerate: A Sequence Boundary Between the Bear Gulch Limestone and Tyler Formations of Central Montana
Abstract
The Serpukhovian Book
Canyon Conglomerate of central Montana is a
newly recognized limestone conglomerate. It overlies and contains
intraformational clasts of the Bear Gulch Limestone, a world-renowned
Carboniferous plattenkalk lagerstätte containing exquisite hard and soft-bodied
fossils. The
Book
Canyon Conglomerate varies in thickness up to 2 meters
over 2 km of laterally discontinuous outcrop. Well logs and cores indicate its
presence beyond the study area in the subsurface between the underlying Bear
Gulch Limestone and overlying Tyler Formation. This conglomerate provides
new information regarding the transition of the marine-dominated Bear Gulch
Limestone to the overlying Tyler Formation, a meandering alluvial valley-fill
within the Big Snowy Trough. Features of the
Book
Canyon Conglomerate
include subaerial/fluvial features such as lateral bars and floodplain paleosol
deposits. Freshwater exposure early in the post-depositional history of Bear
Gulch Limestone explains variations in the contacts between units that
contribute to the debate of
stratigraphic
position. Modern slumping and lack of
datable fossils within the Tyler have complicated studies in the past. Fauna
within the Bear Gulch Limestone are Mississippian, but the Tyler had been
Abstracts are organized as listed in Technical Session (page 27)
Rocky Mountain Section – AAPG: 2019 Annual Meeting 36
previously interpreted as Pennsylvanian. Recent workers with updated
stratigraphic
techniques and additional core have confirmed that the
Mississippian-Pennsylvanian boundary is located within the Tyler Formation,
removing previous concerns over possible age discrepancies. The
Book
Canyon Conglomerate clarifies the Bear Gulch Limestone’s position in time as
a brief marine invasion between the deposition of the lower and upper Tyler
Formations. It represents channels cutting through the Bear Gulch Limestone
due to deepening and shallowing of the Big Snowy Trough, which in past
studies confused its relationship to the Heath and Tyler formations. The
Conglomerate observed in outcrop is in contact with the Tyler Formation and
represents a sequence boundary that confirms core and well log work that
places the Bear Gulch Limestone within the Tyler Formation.
AAPG Datapages/Search and Discovery Article #90357 ©2019 AAPG Rocky Mountain Section Meeting, Cheyenne, Wyoming, September 15-18, 2019