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GeoRef Categories
Era and Period
Epoch and Age
Date
Availability
upright folds
3D geophysical modeling of the Alberton-Mathinna section of the “Main Slide,” northeast Tasmania Available to Purchase
Laramide Uplift near the Ray and Resolution Porphyry Copper Deposits, Southeastern Arizona: Insights into Regional Shortening Style, Magnitude of Uplift, and Implications for Exploration Available to Purchase
Contrasting Structural Styles of Orogenic Gold Deposits, Reefton Goldfield, New Zealand Available to Purchase
Using In Situ SHRIMP U-Pb Monazite and Xenotime Geochronology to Determine the Age of Orogenic Gold Mineralization: An Example from the Paulsens Mine, Southern Pilbara Craton Open Access
Large-scale flat-lying isoclinal folding in extending lithosphere: Santa María de la Alameda dome (Central Iberian Massif, Spain) Open Access
Evolution of the Paleoproterozoic Volcanic-Limestone-Hydrothermal Sediment Succession and Zn-Pb-Ag and Iron Oxide Deposits at Stollberg, Bergslagen Region, Sweden Available to Purchase
STRUCTURAL GEOLOGY OF ROBBEN ISLAND: IMPLICATIONS FOR THE TECTONIC ENVIRONMENT OF SALDANIAN DEFORMATION Available to Purchase
Timing and Structural Controls on Gold Mineralization at the Bogoso Gold Mine, Ghana, West Africa Available to Purchase
The Magdala Lode System, Stawell, Southeastern Australia: Structural Style and Relationship to Gold Mineralization across the Western Lachlan Fold Belt Available to Purchase
Nature of the southwestern boundary of the central Mojave Tertiary province, Rodman Mountains, California Available to Purchase
Evolution of the Starra and Selwyn high-strain zones, Eastern fold belt, Mount Isa Inlier; implications for Au-Cu mineralization Available to Purchase
Deformational History of Eastern Ghat Mobile Belt Around Lathore, Balangir District, Orissa Available to Purchase
Transpression and extensional collapse: Steep belts and flat belts in the Appalachian Central Mobile Belt, northern New Brunswick, Canada Available to Purchase
Thick- and thin-skinned Laramide deformation, Fra Cristobal Range, south-central New Mexico Available to Purchase
The Fra Cristobal Range in south-central New Mexico exposes different styles of deformation variably affecting Precambrian crystalline rocks and Paleozoic, Mesozoic, and Cenozoic cover strata. Three main structural domains are recognized: I is a thick-skinned domain (basement-involved) along the northwest flank of the range; II is a thin-skinned domain along the southwest flank of the range; and III is a combined thick- and thin-skinned domain along the east flank of the range. Domains with thick-skinned deformation are characterized by fault-propagation folds cored by basement blocks bounded by reverse or thrust faults. These domains are segmented by transverse faults into two subdomain types: (1) east-vergent, overturned folds cored by a basement block with corners rounded by cataclastic flow; and (2) upright folds overthrust by basement that is imbricated by east-directed thrust faults. Thin-skinned deformation involves only Paleozoic cover strata and is characterized by decollement-style thrust faults, duplexes, and related upright to overturned folds. Assuming a balance of basement shortening along strike, it is likely that a basement uplift formed west of domain II but is now buried in the Rio Grande rift. Domain II structures developed either as thrusting propagated from basement into cover, by out-of-syncline thrusting east of the uplift, or by gravity sliding off the uplift. Domain III is characterized by a large, east-vergent, overturned monocline (probably basement cored at depth); the overturned limb was subsequently overthrust by its western subhorizontal limb (similar to a cross-crestal fold). A two-stage development is suggested: (1) basement-cored fault-propagation folding in domain III, and (2) shortening in domains I and II to the west and late-stage cross-crestal faulting of the domain III fold. Behavior of basement rocks during deformation includes: (1) shortening and uplift of basement by reverse faulting, (2) cataclastic flow of basement on fault-block corners allowing folding of the basement-cover contact, (3) longitudinal segmentation of some domains by transverse faults, and (4) possible control of basement faulting by preexisting weaknesses.