Matches in SemOpenAlex for { <https://semopenalex.org/work/W2335675534> ?p ?o ?g. }
Showing items 1 to 73 of
73
with 100 items per page.
- W2335675534 endingPage "306" @default.
- W2335675534 startingPage "285" @default.
- W2335675534 abstract "Synopsis The Granophyric Quartz-dolerite is one of a number of intrusions having arcuate outcrops which are concentric with respect to Centre II, Ardnamurchan. It is composed of three rock types: porphyritic dolerite, aphyric dolerite and granophyre. The granophyre extensively net-veins the two kinds of dolerite. However, the development of the net-veining was only the last stage of its intrusive activity. Relationships between granophyre and aphyric dolerite are such as to indicate that at an earlier stage both were in a magmatic state at the same time; that is, they were intruded together, though movement of granophyre magma persisted after the aphyric dolerite had solidified. Evidence is presented to show that intrusion of the porphyritic dolerite was the first episode, and that this provided the host rock for the simultaneous intrusion of aphyric dolerite and granophyre. In its role as host rock, the porphyritic dolerite was at first incompletely crystallized, but for later intrusions it had consolidated. When both dolerites were solid they were net-veined by the granophyre. The inner contact of the Granophyric Quartz-dolerite was formed by a later intrusion. The outer contact for much of its extent dips fairly gently outwards, and it would seem that where this is so intrusion was more nearly in a horizontal than a vertical sense. Locally, sheeted relationships between the three members of the Granophyric Quartz-dolerite, being gently inclined, support this conclusion. There are several possibilities as to the form the intrusion might have, and these are discussed." @default.
- W2335675534 created "2016-06-24" @default.
- W2335675534 creator A5030429765 @default.
- W2335675534 creator A5079050250 @default.
- W2335675534 creator A5088846902 @default.
- W2335675534 date "1966-01-01" @default.
- W2335675534 modified "2023-09-24" @default.
- W2335675534 title "XII.—The Structure and Form of the Granophyric Quartz-Dolerite Intrusion, Centre II, Ardnamurchan, Argyllshire" @default.
- W2335675534 cites W1590598255 @default.
- W2335675534 cites W1968865396 @default.
- W2335675534 cites W2022790962 @default.
- W2335675534 cites W2045144109 @default.
- W2335675534 cites W2065485197 @default.
- W2335675534 cites W2066546562 @default.
- W2335675534 cites W2119275452 @default.
- W2335675534 cites W2133880048 @default.
- W2335675534 cites W2150236857 @default.
- W2335675534 cites W2156391143 @default.
- W2335675534 cites W2321687471 @default.
- W2335675534 cites W2321981993 @default.
- W2335675534 cites W2333414322 @default.
- W2335675534 cites W97709023 @default.
- W2335675534 doi "https://doi.org/10.1017/s0080456800023607" @default.
- W2335675534 hasPublicationYear "1966" @default.
- W2335675534 type Work @default.
- W2335675534 sameAs 2335675534 @default.
- W2335675534 citedByCount "9" @default.
- W2335675534 countsByYear W23356755342016 @default.
- W2335675534 crossrefType "journal-article" @default.
- W2335675534 hasAuthorship W2335675534A5030429765 @default.
- W2335675534 hasAuthorship W2335675534A5079050250 @default.
- W2335675534 hasAuthorship W2335675534A5088846902 @default.
- W2335675534 hasConcept C120806208 @default.
- W2335675534 hasConcept C127313418 @default.
- W2335675534 hasConcept C151730666 @default.
- W2335675534 hasConcept C158251709 @default.
- W2335675534 hasConcept C17409809 @default.
- W2335675534 hasConcept C183222429 @default.
- W2335675534 hasConcept C2779670319 @default.
- W2335675534 hasConcept C2779870107 @default.
- W2335675534 hasConcept C5900021 @default.
- W2335675534 hasConcept C83893233 @default.
- W2335675534 hasConceptScore W2335675534C120806208 @default.
- W2335675534 hasConceptScore W2335675534C127313418 @default.
- W2335675534 hasConceptScore W2335675534C151730666 @default.
- W2335675534 hasConceptScore W2335675534C158251709 @default.
- W2335675534 hasConceptScore W2335675534C17409809 @default.
- W2335675534 hasConceptScore W2335675534C183222429 @default.
- W2335675534 hasConceptScore W2335675534C2779670319 @default.
- W2335675534 hasConceptScore W2335675534C2779870107 @default.
- W2335675534 hasConceptScore W2335675534C5900021 @default.
- W2335675534 hasConceptScore W2335675534C83893233 @default.
- W2335675534 hasIssue "12" @default.
- W2335675534 hasLocation W23356755341 @default.
- W2335675534 hasOpenAccess W2335675534 @default.
- W2335675534 hasPrimaryLocation W23356755341 @default.
- W2335675534 hasRelatedWork W1864929544 @default.
- W2335675534 hasRelatedWork W1990655287 @default.
- W2335675534 hasRelatedWork W2003896462 @default.
- W2335675534 hasRelatedWork W2004738745 @default.
- W2335675534 hasRelatedWork W2016368023 @default.
- W2335675534 hasRelatedWork W2092473008 @default.
- W2335675534 hasRelatedWork W2292017065 @default.
- W2335675534 hasRelatedWork W2315819870 @default.
- W2335675534 hasRelatedWork W2462847736 @default.
- W2335675534 hasRelatedWork W4225006143 @default.
- W2335675534 hasVolume "66" @default.
- W2335675534 isParatext "false" @default.
- W2335675534 isRetracted "false" @default.
- W2335675534 magId "2335675534" @default.
- W2335675534 workType "article" @default.