Matches in SemOpenAlex for { <https://semopenalex.org/work/W2327509780> ?p ?o ?g. }
- W2327509780 abstract "The initial Sr isotopic compositions of acid rocks from world-wide occurrences are plotted against their whole rock isochron ages. They fall within a limited region slightly different from that of assumed source material basaltic magmas. The former has steep inclination than the latter. These two regions intersect at about 3×109 years ago each other. The Rb/Sr value calculated from the inclination of the region of acid rocks is in a range from 0.06 to 0.07, which corresponds to that of andesitic basalt. These may suggest following fact. Namely, the most acid rocks in geologic ages are derived by partial fusion of certain material similar to the chemical composition of andesitic basalt that was already formed by partial fusion of more primitive material probably of peridotitic composition at about 3×100 years ago. This hypothesis seems to be consistent with the geologic evidences that the activities of acid magmas have abruptly increased since about 3×109 years before." @default.
- W2327509780 created "2016-06-24" @default.
- W2327509780 creator A5028389883 @default.
- W2327509780 creator A5038510023 @default.
- W2327509780 date "1972-01-01" @default.
- W2327509780 modified "2023-09-25" @default.
- W2327509780 title "A VIEW ON THE SOURCE MATERIAL OF ACID MAGMAS" @default.
- W2327509780 cites W1502427175 @default.
- W2327509780 cites W1966722927 @default.
- W2327509780 cites W1968337445 @default.
- W2327509780 cites W1971597806 @default.
- W2327509780 cites W1971670231 @default.
- W2327509780 cites W1979476211 @default.
- W2327509780 cites W1979856320 @default.
- W2327509780 cites W1981117492 @default.
- W2327509780 cites W1983145904 @default.
- W2327509780 cites W1985931333 @default.
- W2327509780 cites W1986767557 @default.
- W2327509780 cites W1986897745 @default.
- W2327509780 cites W1992352299 @default.
- W2327509780 cites W1993255325 @default.
- W2327509780 cites W1993483611 @default.
- W2327509780 cites W1995185215 @default.
- W2327509780 cites W1998370907 @default.
- W2327509780 cites W1998691471 @default.
- W2327509780 cites W2001606895 @default.
- W2327509780 cites W2006493918 @default.
- W2327509780 cites W2013865347 @default.
- W2327509780 cites W2013956726 @default.
- W2327509780 cites W2017257982 @default.
- W2327509780 cites W2027528494 @default.
- W2327509780 cites W2028616889 @default.
- W2327509780 cites W2030991149 @default.
- W2327509780 cites W2034459021 @default.
- W2327509780 cites W2038068172 @default.
- W2327509780 cites W2041471679 @default.
- W2327509780 cites W2045558725 @default.
- W2327509780 cites W2048951312 @default.
- W2327509780 cites W2057930319 @default.
- W2327509780 cites W2059542265 @default.
- W2327509780 cites W2059699242 @default.
- W2327509780 cites W2060311516 @default.
- W2327509780 cites W2062009148 @default.
- W2327509780 cites W2063186230 @default.
- W2327509780 cites W2069907781 @default.
- W2327509780 cites W2070088447 @default.
- W2327509780 cites W2073746611 @default.
- W2327509780 cites W2084791384 @default.
- W2327509780 cites W2086156755 @default.
- W2327509780 cites W2086375103 @default.
- W2327509780 cites W2089775759 @default.
- W2327509780 cites W2105400742 @default.
- W2327509780 cites W2105623318 @default.
- W2327509780 cites W2117423497 @default.
- W2327509780 cites W2120072437 @default.
- W2327509780 cites W2121940794 @default.
- W2327509780 cites W2123733168 @default.
- W2327509780 cites W2124362366 @default.
- W2327509780 cites W2133817128 @default.
- W2327509780 cites W2134386441 @default.
- W2327509780 cites W2149579439 @default.
- W2327509780 cites W2156860638 @default.
- W2327509780 cites W2156964216 @default.
- W2327509780 cites W2159247473 @default.
- W2327509780 cites W2164242582 @default.
- W2327509780 cites W2320377128 @default.
- W2327509780 cites W2320849684 @default.
- W2327509780 cites W2321954463 @default.
- W2327509780 cites W2328785567 @default.
- W2327509780 cites W2332996341 @default.
- W2327509780 cites W2785235427 @default.
- W2327509780 doi "https://doi.org/10.2465/ganko1941.67.11" @default.
- W2327509780 hasPublicationYear "1972" @default.
- W2327509780 type Work @default.
- W2327509780 sameAs 2327509780 @default.
- W2327509780 citedByCount "0" @default.
- W2327509780 crossrefType "journal-article" @default.
- W2327509780 hasAuthorship W2327509780A5028389883 @default.
- W2327509780 hasAuthorship W2327509780A5038510023 @default.
- W2327509780 hasBestOaLocation W23275097801 @default.
- W2327509780 hasConcept C120806208 @default.
- W2327509780 hasConcept C127313418 @default.
- W2327509780 hasConcept C151730666 @default.
- W2327509780 hasConcept C161509811 @default.
- W2327509780 hasConcept C162973429 @default.
- W2327509780 hasConcept C17409809 @default.
- W2327509780 hasConcept C192241223 @default.
- W2327509780 hasConcept C1965285 @default.
- W2327509780 hasConcept C199289684 @default.
- W2327509780 hasConcept C36986328 @default.
- W2327509780 hasConcept C46381822 @default.
- W2327509780 hasConcept C487381 @default.
- W2327509780 hasConcept C77928131 @default.
- W2327509780 hasConceptScore W2327509780C120806208 @default.
- W2327509780 hasConceptScore W2327509780C127313418 @default.
- W2327509780 hasConceptScore W2327509780C151730666 @default.
- W2327509780 hasConceptScore W2327509780C161509811 @default.
- W2327509780 hasConceptScore W2327509780C162973429 @default.
- W2327509780 hasConceptScore W2327509780C17409809 @default.
- W2327509780 hasConceptScore W2327509780C192241223 @default.