4 edition of Cordilleran metamorphic core complexes. Edited by Max D. Crittenden, Jr. [and others] found in the catalog.
|LC Classifications||QE 79 C795 1980|
|The Physical Object|
|Pagination||490 p. ill., maps|
|Number of Pages||490|
The Shuswap MCC is the largest of the Cordilleran metamorphic core complexes (MCC) (Crittenden et al. ) and straddles the suture between allochthonous terranes and the North American High-strain mylonitic rocks in Cordilleran metamorphic core complexes reflect ductile deformation in the middle crust, but in many examples it is unclear how these mylonites relate to the brittle
Algorithms for floating-point arithmetic are presented throughout the book and illustrated where possible by example programs which show how these techniques appear in actual coding and volume itself breaks its core topic into four parts: the Web view.  The Mohave Mountains lie within the belt of Cordilleran metamorphic core complexes [Coney, ; Crittenden et al., ; Davis and Lister, ]. The structural setting is a zone of highly extended and tilted fault blocks, which Howard and John defined as the Colorado River extensional ://
A 'read' is counted each time someone views a publication summary (such as the title, abstract, and list of authors), clicks on a figure, or views or downloads the ://  The Ruby Mountains metamorphic core complex is a well studied structure in NE Nevada [e.g., Snoke, ; Dallmeyer et al., ; Dokka et al., ; Mueller and Snoke, ; McGrew and Snee, ; McGrew et al., ]. The complex was exhumed along a west‐dipping mylonitic detachment that is exposed sporadically along the western
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Growing evidence shows that these metamorphic terranes and related features evolved in part during early to middle Tertiary time (55 to 15 m.y. B.P.), that is, after the Laramide orogeny but before basin-range faulting.
These terranes have been termed "metamorphic core complexes." Cordilleran Metamorphic Core Complexes Author(s) Max D. Crittenden, Jr.; Max D. Crittenden, Jr. Search for other works by this author on: GSW. Google Scholar. Peter J. Coney; Peter J.
Coney Search for other works by this author on: Max D. Crittenden, Jr., "Metamorphic core complexes of the North American Cordillera: Summary", Cordilleran Metamorphic Core Complexes, Max D. Crittenden, Jr ISBN: OCLC Number: Description: vi, pages: illustrations ; 27 cm. Contents: Dedication to Peter Misch --Part uction and overview --Introduction / Peter J.
Coney --Cordilleran metamorphic core complexes: an overview / Peter J. Coney --Part rn Basin and Range --Structural characteristics of metamorphic core complexes, southern Arizona ISBN: OCLC Number: Description: vi, p.: ill. ; 27 cm. Contents: Dedication to Peter Misch --Part uction and overview --Introduction / Peter J.
Coney --Cordilleran metamorphic core complexes: an overview / Peter J. Coney --Part rn Basin and Range --Structural characteristics of metamorphic core complexes, southern Arizona / George H hinterland metamorphic rocks and the thrust belt to the east.
This conference was followed by a Geological Society of America symposium, organized by Max. on the same subject. Along with Peter J. Coney and George H. Davis, in Max edited a Geological Society of America Memoir on Cordilleran metamorphic core :// Cordilleran metamorphic core complexes edited by Max D.
Crittenden, Jr., Peter J. Coney, George H. Davis Geological Society of America George H. Davis is the author of Structural Geology of Rocks and Regions ( avg rating, 59 ratings, 1 review, published ), by George ( avg rat Eric S. Cheney, "Kettle dome and related structures of northeastern Washington", Cordilleran Metamorphic Core Complexes, Max D.
Crittenden, Jr., Peter J. Coney Geologic data at several core complexes have been used to infer very high slip rates (8–30 mm/a) on these faults [e.g., Lister and Davis, ]. High estimates of both slip magnitude and rate at many core complexes have greatly contributed to the interpretation of these features as unique modes of crustal extension not active in modern :// Analysis of shear criteria enables the kinematics of two main ductile-shearing events (D 1 and D 2) to be established in the Raft River, Grouse Creek and Albion ‘metamorphic core complex’.The first event (D 1) is a NNE-thrusting and corresponds to Mesozoic shortening.A well developed non-coaxial ductile deformation (D 2), of Cenozoic age, is marked by the occurrence of opposing eastward change in the bulk movement picture, the exact details Rocks similar to the S-C mylonites described by of the timing relationship may be of less significance thanBerth6 et al.
() occur throughout the Cordilleran the S-C relationship rphic core complexes in Arizona, California, Type I S-C mylonites have widespread occurrence METAMORPHIC CORE COMPLEXES OF THE SOUTHWESTERN UNITED STATES - AN UPDATED ANALYSIS William A Rehrig there are authors, in the volume edited by Crittenden, Coney, and Davis ().
organized by M. Crittenden, Jr., P. Coney, The North American Cordillera, including the Sevier and Laramide belts, forms one of Earth's classic orogenic systems, providing a natural laboratory for seminal studies that have advanced our understanding of thrust kinematics and mechanics (e.g., Rubey and Hubert,Dahlstrom,Price and Mountjoy,Burchfiel and Davis,Boyer and Elliott, ), synconvergent extension of Metamorphic core complexes evolved in the western Cordillera in early to middle Tertiary time as a response to profound regional extension and thermal incursion; the deformation was punctuated by Click on the book chapter title to read :// X-ray texture goniometry operated in the transmission mode has been applied to fine-grained, phyllosilicate-rich SC-mylonites from the Santa Rosa mylo I also strongly recommend "Continental Deformation" edited by Hancock.
This book is a collection of 18 review papers each of them written by renowned geoscientists. For each topic I suggest, for those of you who are really keen on tectonics, to read a few scientific papers () from the list provided. The exhumation of the Menderes massif metamorphic core complex in Western Anatolia.
Terra Abstracts 5, Wernicke, B., Low-angle normal faults in the Basin and Range province: nappe tectonics in an extending orogen. Nature– Whitney, D.L., Bozkurt, E., Metamorphic history of the southern Menderes massif, western :// Methods of deducing slip-line orientations from the geometry of folds.
Carnegie Institution of Washington Year B Haxel, G. & Dillon, J. The Pe[ona-Orocopia Schist and Vincent-Chocolate Mountain thrust system, southern California. In: Mesozoic Paleogeography of the Western United States (edited by Howell, D.
G. & McDougall northwest zone of metamorphic core complexes in Arizona: Geological Society of Americ~ Abstracts with Programs, v. 9, no. 7, p. _____- and Reynolds, S.
J.,Geolo~ic and geochronologic reconnaissance of a north west-trending zone of metamorphic complexes in southern Arizona: Geological Society of America Memoirp.