Matches in SemOpenAlex for { <https://semopenalex.org/work/W2296637161> ?p ?o ?g. }
Showing items 1 to 78 of
78
with 100 items per page.
- W2296637161 endingPage "130" @default.
- W2296637161 startingPage "123" @default.
- W2296637161 abstract "ABSTRACT The structural geology of British Mountains, Yukon, between Crow and Spring rivers is characterized by a series of high-angle (about 30°) thrust faults that are parallel to each other and to the mountain front, trend in a northwesterly direction, and dip to the southwest. The thrusts have been traced in the field over a distance of 10 mi. They are difficult to detect on the available high-altitude aerial photographs but, once located in the field, the ridges (which are their most common topographic expression) can be traced on the photographs. Two stratigraphic units are involved in the faulting. Unfossiliferous quartzites, argillites, and limestones assigned to the Neruokpuk Formation, believed to range in age from late Proterozoic to early Devonian, form the hanging wall of the faults. Where the thrusts can be detected, the foot-wall is a limestone or a calcareous chert-pebble conglomerate of the Triassic Shublik Formation, which can be identified by the common presence of the pelecypod Monotis sp. The Triassic beds can be seen to lie unconformably on Neruokpuk strata. At most only 50 feet of the lowest part of the Shublik Formation is preserved in the footwall of the faults. The amount of movement along the thrusts is unknown but it is believed not to be great, meaning that it is measurable in hundreds of feet rather than in miles. To the northwest and southeast of the area between Crow and Spring rivers, the Shublik Formation is absent and the thrusts are not traceable but seem to disappear in the Neruokpuk Formation. Thrusting is believed to have taken place during the Cretaceous and to represent a phase of the Laramide Revolution." @default.
- W2296637161 created "2016-06-24" @default.
- W2296637161 creator A5053788322 @default.
- W2296637161 date "1973-03-01" @default.
- W2296637161 modified "2023-09-26" @default.
- W2296637161 title "Geology of Crow River - Spring River Area British Mountain Front Yukon, Canada1" @default.
- W2296637161 doi "https://doi.org/10.35767/gscpgbull.21.1.123" @default.
- W2296637161 hasPublicationYear "1973" @default.
- W2296637161 type Work @default.
- W2296637161 sameAs 2296637161 @default.
- W2296637161 citedByCount "0" @default.
- W2296637161 crossrefType "journal-article" @default.
- W2296637161 hasAuthorship W2296637161A5053788322 @default.
- W2296637161 hasConcept C106804226 @default.
- W2296637161 hasConcept C107832698 @default.
- W2296637161 hasConcept C110041135 @default.
- W2296637161 hasConcept C111368507 @default.
- W2296637161 hasConcept C114793014 @default.
- W2296637161 hasConcept C127313418 @default.
- W2296637161 hasConcept C127413603 @default.
- W2296637161 hasConcept C151730666 @default.
- W2296637161 hasConcept C173776410 @default.
- W2296637161 hasConcept C175551986 @default.
- W2296637161 hasConcept C2777551076 @default.
- W2296637161 hasConcept C2777760186 @default.
- W2296637161 hasConcept C2778712887 @default.
- W2296637161 hasConcept C6494504 @default.
- W2296637161 hasConcept C77928131 @default.
- W2296637161 hasConcept C78519656 @default.
- W2296637161 hasConcept C93033518 @default.
- W2296637161 hasConceptScore W2296637161C106804226 @default.
- W2296637161 hasConceptScore W2296637161C107832698 @default.
- W2296637161 hasConceptScore W2296637161C110041135 @default.
- W2296637161 hasConceptScore W2296637161C111368507 @default.
- W2296637161 hasConceptScore W2296637161C114793014 @default.
- W2296637161 hasConceptScore W2296637161C127313418 @default.
- W2296637161 hasConceptScore W2296637161C127413603 @default.
- W2296637161 hasConceptScore W2296637161C151730666 @default.
- W2296637161 hasConceptScore W2296637161C173776410 @default.
- W2296637161 hasConceptScore W2296637161C175551986 @default.
- W2296637161 hasConceptScore W2296637161C2777551076 @default.
- W2296637161 hasConceptScore W2296637161C2777760186 @default.
- W2296637161 hasConceptScore W2296637161C2778712887 @default.
- W2296637161 hasConceptScore W2296637161C6494504 @default.
- W2296637161 hasConceptScore W2296637161C77928131 @default.
- W2296637161 hasConceptScore W2296637161C78519656 @default.
- W2296637161 hasConceptScore W2296637161C93033518 @default.
- W2296637161 hasIssue "1" @default.
- W2296637161 hasLocation W22966371611 @default.
- W2296637161 hasOpenAccess W2296637161 @default.
- W2296637161 hasPrimaryLocation W22966371611 @default.
- W2296637161 hasRelatedWork W135500546 @default.
- W2296637161 hasRelatedWork W1484439612 @default.
- W2296637161 hasRelatedWork W1521588668 @default.
- W2296637161 hasRelatedWork W1525158452 @default.
- W2296637161 hasRelatedWork W1532354473 @default.
- W2296637161 hasRelatedWork W1939284209 @default.
- W2296637161 hasRelatedWork W1965809649 @default.
- W2296637161 hasRelatedWork W1965911695 @default.
- W2296637161 hasRelatedWork W2010720688 @default.
- W2296637161 hasRelatedWork W2028356286 @default.
- W2296637161 hasRelatedWork W2031169777 @default.
- W2296637161 hasRelatedWork W2064466388 @default.
- W2296637161 hasRelatedWork W2083090240 @default.
- W2296637161 hasRelatedWork W2095272615 @default.
- W2296637161 hasRelatedWork W2130098307 @default.
- W2296637161 hasRelatedWork W2147147544 @default.
- W2296637161 hasRelatedWork W2211593422 @default.
- W2296637161 hasRelatedWork W2268513576 @default.
- W2296637161 hasRelatedWork W2277060753 @default.
- W2296637161 hasRelatedWork W3248433 @default.
- W2296637161 hasVolume "21" @default.
- W2296637161 isParatext "false" @default.
- W2296637161 isRetracted "false" @default.
- W2296637161 magId "2296637161" @default.
- W2296637161 workType "article" @default.