Zobrazeno 1 - 10
of 71
pro vyhledávání: '"D. F Strong"'
Publikováno v:
Chemical Geology. 83:119-132
A procedure has been developed for the routine determination of the precious metals (Ru, Rh, Pd, Os, Ir, Pt and Au) in geological materials using inductively coupled plasma-mass spectrometry (ICP-MS). The precious metals were isolated using a combina
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a0a85ffdd20e856382fbfd800f68f0d
https://doi.org/10.1016/0009-2541(90)90144-v
https://doi.org/10.1016/0009-2541(90)90144-v
Publikováno v:
Atlantic Geology. 27
In order to evaluate the late-stage physical and chemical evolution of the Upper Devonian, peraluminous South Mountain Batholith, mineral chemistry (muscovite, feldspars), oxygen isotopes (whole rock, mineral separates) and Al/Si ordering of K-feldsp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44487ed0ce6dee3fdbddc568961d7696
https://doi.org/10.4138/1718
https://doi.org/10.4138/1718
Publikováno v:
Equilibrium and Kinetics in Contact Metamorphism ISBN: 9783642761478
Variations in stable isotope ratios can be particularly helpful in studying the origins of igneous rocks, as well as the fluid interactions that may accompany magma generation or which may occur during and after magma emplacement and solidification (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::070f214685872109f1ea04cff3e1d2d3
https://doi.org/10.1007/978-3-642-76145-4_17
https://doi.org/10.1007/978-3-642-76145-4_17
Publikováno v:
Avalonian and Cadomian Geology of the North Atlantic ISBN: 9789401066679
Avalonian and Cadomian Geology of the North Atlantic
Avalonian and Cadomian Geology of the North Atlantic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::99083a6586d837509f07a4a2ed9aa664
https://doi.org/10.1007/978-94-009-0401-9_9
https://doi.org/10.1007/978-94-009-0401-9_9
Autor:
R. A. Jamieson, D. F. Strong
Publikováno v:
American Journal of Science. 281:264-281
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f081bb200ec1823f472b59edefa3ec34
https://doi.org/10.2475/ajs.281.3.264
https://doi.org/10.2475/ajs.281.3.264
Autor:
D. F. Strong, Jaroslav Dostal
Publikováno v:
Contributions to Mineralogy and Petrology. 72:165-173
Rare Earth Element (REE) data confirm earlier suggestions from major and trace elements that the Proterozoic Burin Group in the southwestern Avalon Zone is similar to modern oceanic tholeiites, and also exhibit a systematic evolution through the sequ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a15fc4e073762e862b42d17fc69a075b
https://doi.org/10.1007/bf00399476
https://doi.org/10.1007/bf00399476
Autor:
W. L. Dickson, D. F Strong
Publikováno v:
Canadian Journal of Earth Sciences. 15:145-156
Granitoid plutons of similar (Silurian–Devonian) age intrude four of the tectono-stratigraphic zones of northeastern Newfoundland, and show systematic petrographic and chemical differences corresponding to the tectonic zone in which they occur. Tho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0727ef1183969b858646f6601dab8e5b
https://doi.org/10.1139/e78-012
https://doi.org/10.1139/e78-012
Autor:
D. F. Strong, H. C. Teng
Publikováno v:
Canadian Journal of Earth Sciences. 13:1374-1385
The southern part of the Burin Peninsula of southeast Newfoundland is marked by extensive Carboniferous granite magmatism, intruding Late Precambrian to Middle Cambrian volcanic and sedimentary rocks. The St. Lawrence pluton, representative of this C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::69d99d83b0f69e40b8135f4d2a23f2df
https://doi.org/10.1139/e76-142
https://doi.org/10.1139/e76-142
Publikováno v:
Canadian Journal of Earth Sciences. 14:456-476
Whole-rock Rb–Sr isochron ages from nine granitic plutons that intrude the Central Mobile Belt and the Avalon Zone of Newfoundland are consistent with the view that most of the magmatic activity for this segment of the Appalachian Orogen is related
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0f3642094d257b432c00bbe22437affe
https://doi.org/10.1139/e77-045
https://doi.org/10.1139/e77-045