FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2024809700> ?p ?o ?g. }

• W2024809700 endingPage "886" @default.
• W2024809700 startingPage "861" @default.
• W2024809700 abstract "The Highland Range of southern Nevada contains a major anticline and syncline that constitute the westernmost segments of the Black Mountains accommodation zone in the highly extended Colorado River extensional corridor. The folds are defined by thick tilted sections of Miocene volcanic and sedimentary strata that accumulated immediately prior to and during regional extension. The folds are generally symmetrical, with interlimb angles that exceed 90°, subhorizontal hingelines, and steeply inclined axial surfaces. East- and west-dipping normal faults dominate the west- and east-tilted limbs of the folds, respectively. The limbs of the folds are parts of major half grabens. Tilt fanning within these half grabens and 15 new 40Ar/39Ar dates bracket major extension between about 16.5 and 11 Ma. Tilting of the opposing fold limbs occurred simultaneously and was contemporaneous with extension. The anticline and syncline are therefore interpreted as fault-related extensional folds produced by the partial, along-strike overlap of oppositely dipping normal-fault systems and attendant tilt-block domains. The anticline developed between overlapping listric normal faults that dip toward one another, including the east-dipping McCullough Range and west-dipping Keyhole Canyon faults. Each limb of the anticline is a rollover fold developed in the hanging wall of the inwardly dipping listric normal faults. The syncline formed between overlapping outwardly dipping listric faults, as adjacent fault blocks were tilted toward one another. The dominant folding style was fault-bend folding, with drag-folding and displacement-gradient folding playing subsidiary roles. The anticline and syncline significantly affected depositional patterns, with synextensional units, including two major ash-flow tuffs, thinning toward the anticlinal hinge and thickening toward the synclinal hinge. The Black Mountains accommodation zone is largely composed of intersecting northwest-trending anticlines and northeast-trending synclines, both occurring at a variety of scales depending on the amount of overlap between the opposing normal-fault systems. This three-dimensional geometry contrasts with the typical style of folding in contractional settings and may characterize extensional accommodation zones that include the partial along-strike overlap of multiple, oppositely dipping normal faults. The folds in the Highland Range serve as well-exposed analogues of similar features in hydrocarbon-rich areas of submerged continental margins." @default.
• W2024809700 created "2016-06-24" @default.
• W2024809700 creator A5020180060 @default.
• W2024809700 creator A5039782957 @default.
• W2024809700 creator A5070391035 @default.
• W2024809700 creator A5090111027 @default.
• W2024809700 date "2002-04-01" @default.
• W2024809700 modified "2023-10-17" @default.
• W2024809700 title "Miocene extension and fault-related folding in the Highland Range, southern Nevada: a three-dimensional perspective" @default.
• W2024809700 cites W1769048309 @default.
• W2024809700 cites W1904477933 @default.
• W2024809700 cites W1965396277 @default.
• W2024809700 cites W1968427238 @default.
• W2024809700 cites W1970474278 @default.
• W2024809700 cites W1974334364 @default.
• W2024809700 cites W1978216542 @default.
• W2024809700 cites W1981284128 @default.
• W2024809700 cites W1984706520 @default.
• W2024809700 cites W1996132723 @default.
• W2024809700 cites W1997167319 @default.
• W2024809700 cites W2005440355 @default.
• W2024809700 cites W2008301502 @default.
• W2024809700 cites W2017649492 @default.
• W2024809700 cites W2020505977 @default.
• W2024809700 cites W2022223654 @default.
• W2024809700 cites W2022392030 @default.
• W2024809700 cites W2031903193 @default.
• W2024809700 cites W2045766527 @default.
• W2024809700 cites W2050442970 @default.
• W2024809700 cites W2051220980 @default.
• W2024809700 cites W2052204780 @default.
• W2024809700 cites W2072385009 @default.
• W2024809700 cites W2074093419 @default.
• W2024809700 cites W2074206445 @default.
• W2024809700 cites W2081172802 @default.
• W2024809700 cites W2082713797 @default.
• W2024809700 cites W2092393488 @default.
• W2024809700 cites W2092995835 @default.
• W2024809700 cites W2098891607 @default.
• W2024809700 cites W2102850028 @default.
• W2024809700 cites W2112708812 @default.
• W2024809700 cites W2114873327 @default.
• W2024809700 cites W2120031454 @default.
• W2024809700 cites W2121733203 @default.
• W2024809700 cites W2124474119 @default.
• W2024809700 cites W2126373657 @default.
• W2024809700 cites W2127136348 @default.
• W2024809700 cites W2129513811 @default.
• W2024809700 cites W2131822747 @default.
• W2024809700 cites W2133701145 @default.
• W2024809700 cites W2139732287 @default.
• W2024809700 cites W2142981515 @default.
• W2024809700 cites W2143647645 @default.
• W2024809700 cites W2144520928 @default.
• W2024809700 cites W2145604970 @default.
• W2024809700 cites W2149165653 @default.
• W2024809700 cites W2152832284 @default.
• W2024809700 cites W2164186072 @default.
• W2024809700 cites W2164896055 @default.
• W2024809700 cites W2178484906 @default.
• W2024809700 cites W2306169434 @default.
• W2024809700 cites W2315393910 @default.
• W2024809700 cites W2333145890 @default.
• W2024809700 cites W2338594170 @default.
• W2024809700 cites W2339991708 @default.
• W2024809700 cites W2340347543 @default.
• W2024809700 cites W2342564574 @default.
• W2024809700 cites W2479330942 @default.
• W2024809700 cites W3123620808 @default.
• W2024809700 cites W3159271348 @default.
• W2024809700 doi "https://doi.org/10.1016/s0191-8141(01)00116-x" @default.
• W2024809700 hasPublicationYear "2002" @default.
• W2024809700 type Work @default.
• W2024809700 sameAs 2024809700 @default.
• W2024809700 citedByCount "33" @default.
• W2024809700 countsByYear W20248097002012 @default.
• W2024809700 countsByYear W20248097002013 @default.
• W2024809700 countsByYear W20248097002014 @default.
• W2024809700 countsByYear W20248097002017 @default.
• W2024809700 countsByYear W20248097002018 @default.
• W2024809700 countsByYear W20248097002019 @default.
• W2024809700 countsByYear W20248097002022 @default.
• W2024809700 countsByYear W20248097002023 @default.
• W2024809700 crossrefType "journal-article" @default.
• W2024809700 hasAuthorship W2024809700A5020180060 @default.
• W2024809700 hasAuthorship W2024809700A5039782957 @default.
• W2024809700 hasAuthorship W2024809700A5070391035 @default.
• W2024809700 hasAuthorship W2024809700A5090111027 @default.
• W2024809700 hasConcept C114793014 @default.
• W2024809700 hasConcept C116637073 @default.
• W2024809700 hasConcept C127313418 @default.
• W2024809700 hasConcept C127413603 @default.
• W2024809700 hasConcept C136137745 @default.
• W2024809700 hasConcept C144027150 @default.
• W2024809700 hasConcept C149465734 @default.
• W2024809700 hasConcept C151730666 @default.
• W2024809700 hasConcept C165205528 @default.
• W2024809700 hasConcept C166839181 @default.

• next