Matches in SemOpenAlex for { <https://semopenalex.org/work/W2225211020> ?p ?o ?g. }
Showing items 1 to 62 of
62
with 100 items per page.
- W2225211020 endingPage "60" @default.
- W2225211020 startingPage "60" @default.
- W2225211020 abstract "Abstract The Ouachita structural belt in Texas, buried for about 850 miles of its 900-mile course, can be divided into two main segments. The northern limb of the belt, extending from the Ouachita Mountains of Oklahoma to central Texas, is clearly an extension of the Ouachita Mountains, It is composed of: (1) A frontal zone of essentially unmetamorphosed folded and thrustfaulted rocks which are mostly Stanley shale and sandstone; slices of pre-Stanley rocks are present along the course of the front and in places Ouachita facies rocks are thrust over foreland facies rocks; (2) an intermediate zone of very weakly metamorphosed dark clastic rocks; and (3) an eastern zone of highly sheared phyllites, slates, and metaquartzites which is interpreted as thrust over the frontal and intermediate zones. The tectonic break demarking the western edge of the highly sheared rocks may be analogous to the Blue Ridge front in the Appalachian system. The western limb of the Ouachita structural belt, extending from the Llano uplift westward to the Marathon area and thence southward into Mexico, is markedly different from the north limb. Immediately west of the Llano uplift in the eastern Kerr basin, lower Paleozoic Ouachita facies rocks appear to be thrust over foreland sediments; farther west there are indications that there is a major re-entrant in the Ouachita front and that the Kerr basin extends southward to include most of Uvalde and Medina counties; in Kinney, Val Verde, and Terrell counties highly sheared rocks have overridden the frontal zone of the belt and rest on foreland facies rocks; in Brewster County the frontal zone is exposed in the Marathon salient which at least in its northern part is allochthonous. Structural interpretation of the western limb is still tentative. The Ouchita system was a major mobile belt extending along the southern margin of the North American continent throughout most of Paleozoic time; its present course was determined by the shape of the craton against which it was deformed." @default.
- W2225211020 created "2016-06-24" @default.
- W2225211020 creator A5048193202 @default.
- W2225211020 date "1958-01-01" @default.
- W2225211020 modified "2023-09-23" @default.
- W2225211020 title "The Subsurface Ouachita Structural Belt in Texas: Abstract" @default.
- W2225211020 hasPublicationYear "1958" @default.
- W2225211020 type Work @default.
- W2225211020 sameAs 2225211020 @default.
- W2225211020 citedByCount "0" @default.
- W2225211020 crossrefType "journal-article" @default.
- W2225211020 hasAuthorship W2225211020A5048193202 @default.
- W2225211020 hasConcept C109007969 @default.
- W2225211020 hasConcept C114793014 @default.
- W2225211020 hasConcept C127313418 @default.
- W2225211020 hasConcept C13106087 @default.
- W2225211020 hasConcept C146588470 @default.
- W2225211020 hasConcept C151730666 @default.
- W2225211020 hasConcept C17409809 @default.
- W2225211020 hasConcept C193748577 @default.
- W2225211020 hasConcept C2780103627 @default.
- W2225211020 hasConcept C77928131 @default.
- W2225211020 hasConceptScore W2225211020C109007969 @default.
- W2225211020 hasConceptScore W2225211020C114793014 @default.
- W2225211020 hasConceptScore W2225211020C127313418 @default.
- W2225211020 hasConceptScore W2225211020C13106087 @default.
- W2225211020 hasConceptScore W2225211020C146588470 @default.
- W2225211020 hasConceptScore W2225211020C151730666 @default.
- W2225211020 hasConceptScore W2225211020C17409809 @default.
- W2225211020 hasConceptScore W2225211020C193748577 @default.
- W2225211020 hasConceptScore W2225211020C2780103627 @default.
- W2225211020 hasConceptScore W2225211020C77928131 @default.
- W2225211020 hasLocation W22252110201 @default.
- W2225211020 hasOpenAccess W2225211020 @default.
- W2225211020 hasPrimaryLocation W22252110201 @default.
- W2225211020 hasRelatedWork W1541447652 @default.
- W2225211020 hasRelatedWork W2019013341 @default.
- W2225211020 hasRelatedWork W2049062037 @default.
- W2225211020 hasRelatedWork W2057734856 @default.
- W2225211020 hasRelatedWork W2073580995 @default.
- W2225211020 hasRelatedWork W2086900601 @default.
- W2225211020 hasRelatedWork W2099596799 @default.
- W2225211020 hasRelatedWork W2108416038 @default.
- W2225211020 hasRelatedWork W2118940376 @default.
- W2225211020 hasRelatedWork W2120234406 @default.
- W2225211020 hasRelatedWork W2122017754 @default.
- W2225211020 hasRelatedWork W2129588771 @default.
- W2225211020 hasRelatedWork W2131347338 @default.
- W2225211020 hasRelatedWork W2166411572 @default.
- W2225211020 hasRelatedWork W2169671053 @default.
- W2225211020 hasRelatedWork W2276143419 @default.
- W2225211020 hasRelatedWork W2281667049 @default.
- W2225211020 hasRelatedWork W2517054845 @default.
- W2225211020 hasRelatedWork W2043152309 @default.
- W2225211020 hasRelatedWork W2183677482 @default.
- W2225211020 hasVolume "26" @default.
- W2225211020 isParatext "false" @default.
- W2225211020 isRetracted "false" @default.
- W2225211020 magId "2225211020" @default.
- W2225211020 workType "article" @default.