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pro vyhledávání: '"Larry T. Middleton"'
Autor:
Larry T. Middleton
Publikováno v:
Rocky Mountain Geology. 36:81-98
Middle and Upper Cambrian strata in western Wyoming and throughout the Rocky Mountain region comprise relatively thick successions of nearshore and shelf siliciclastics and carbonates deposited during numerous marine transgressions and regressions. T
Publikováno v:
Geological Society of America Bulletin. 103:472-485
The stratigraphy, provenance, and structural involvement of tectogenic sedimentary rocks along the southern and western margins of the Wind River Range in western Wyoming record a complex Laramide and later uplift history and identify the timing and
Publikováno v:
Mountain Geologist. 23:19-25
The established mid-Tertiary stratigraphy along the southern margin of the Wind River Range is of questionable chronologic validity because of the difficulty in discriminating among the several tuffaceous units and because lithologic criteria have be
Publikováno v:
Quaternary Research. 27:323-331
The extinct Harrington's mountain goat (Oreamnos harringtoni Stock) is predominantly known from dry cave localities in the Grand Canyon, Arizona, in addition to two sites in the Great Basin, Nevada, and from San Josecito Cave, Nuevo Leon, Mexico. A d
Publikováno v:
AAPG Bulletin. 67
Surface observations along the southern margin of the Wind River Range in Fremont County, Wyoming, indicate that early motion along the Wind River and Continental faults controlled depositional patterns and lithologic characteristics of the local syn
Publikováno v:
AAPG Bulletin. 64
Middle and Upper Cambrian deposits in Wyoming represent a classic transgression or onlapping sequence of clastic and non-clastic rocks. However, sedimentologic and paleontologic criteria indicate deposition in a variety of shallow-marine, nearshore e
Autor:
Larry T. Middleton, Ronald C. Blakey
Publisher Summary This chapter describes the processes and controls on the intertonguing of the Kayenta and Navajo formations in northern Arizona. The Kayenta comprises a heterogeneous assemblage of coarse- to fine-grained clastics that crop out in w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::41ad3e655d23cc79f2fe985e4c2062f7
https://doi.org/10.1016/s0070-4571(08)70815-x
https://doi.org/10.1016/s0070-4571(08)70815-x