Zobrazeno 1 - 10
of 17
pro vyhledávání: '"C. C. Rundle"'
Autor:
Stephen R. Noble, T. S. Brewer, C. C. Rundle, C. J. Evans, D. W. Holliday, Tim Pharaoh, Richard J. Merriman, G. S. Kimbell, J. M. Allsop
Publikováno v:
Proceedings of the Yorkshire Geological Society. 51:329-342
SUMMARY A granophyric microgranite has been proved in the sub-Carboniferous basement at Moorby, near Horncastle in south Lincolnshire. The microgranite is interpreted as a high level intrusion which has suffered strong alteration and deformation subs
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c737519bd31ec4ed9397c056173ea39c
https://doi.org/10.1144/pygs.51.4.329
https://doi.org/10.1144/pygs.51.4.329
Publikováno v:
Journal of the Geological Society. 153:33-38
U-Pb analyses of zircons from the Ennerdale granitic intrusion and Eskdale Granite (English Lake District) give ages of 452 ± 4 Ma and 450 ± 3 Ma respectively. These data confirm the sub-volcanic association of these intrusions, and show that previ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8b05e87467462674559e4f652ec4f0ce
https://doi.org/10.1144/gsjgs.153.1.0033
https://doi.org/10.1144/gsjgs.153.1.0033
Publikováno v:
Journal of Geophysical Research: Solid Earth. 99:21705-21715
Mechanical analysis of lithospheric deformation associated with an intracontinental transform fault suggests that it should be associated with a pattern of vertical axis rotations governed by the length of the fault, its displacement, and the mechani
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dfde65306e0e0cca573b8ad7ad38f3bf
https://doi.org/10.1029/94jb01665
https://doi.org/10.1029/94jb01665
Publikováno v:
Journal of the Geological Society. 148:861-868
The Central Belt of the Southern Uplands Terrane, in both Scotland and Ireland, is a faulted and imbricated sequence of Caradoc to Llandovery shales and Llandovery turbidites with numerous interbedded K-bentonites. The bentonites are composed dominan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a6cf5e90fd5034ad76357ec68401d36d
https://doi.org/10.1144/gsjgs.148.5.0861
https://doi.org/10.1144/gsjgs.148.5.0861
Publikováno v:
The Journal of Geology. 94:505-522
Siluro-Devonian magmatism in the Southern Uplands (Scotland) and Northern Ireland includes a hitherto neglected regional SW-NE zone, c. 10 km wide and >300 km long, of calc-alkaline lamprophyre dykes. Lamprophyres were locally emplaced contemporaneou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0e914d5d07d607e7bc45fe08af0bb635
https://doi.org/10.1086/629054
https://doi.org/10.1086/629054
Publikováno v:
Journal of the Geological Society. 138:31-46
Sills of olivine-microgabbro and olivine-dolerite 0.5–180 m thick intrude Lower Liassic (Hettangian–Sinemurian) sediments in the Fastnet Basin, a SW extension of the N Celtic Sea Basin, about Lat. 50°N, Long. 10°W. The evidence of 3 wells and 2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dfa0d3343aab4c9989a3187f1e9ee814
https://doi.org/10.1144/gsjgs.138.1.0031
https://doi.org/10.1144/gsjgs.138.1.0031
Autor:
P. M. Allen, N. J. Fortey, Anthony H. Cooper, B. C. Webb, C. C. Rundle, M. K. Lee, D. C. Cooper
Publikováno v:
Journal of the Geological Society. 145:523-540
The Crummock Water aureole, an ENE-trending elongate zone of bleached and recrystallized Skiddaw Group rocks, 24 km in length and up to 3 km wide, is a zone in which pervasive metasomatism has modified the composition of the dominantly siltstone and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da8325858b60810b7bec1ca8cdd876f7
https://doi.org/10.1144/gsjgs.145.4.0523
https://doi.org/10.1144/gsjgs.145.4.0523
Autor:
C. C. Rundle, N. J. Snelling
Publikováno v:
Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. 286:567-583
Uranium and lead analyses of rock samples from the Witwatersrand, Ventersdorp, and Transvaal supergroups give mainly discordant ages. Samples from the Upper Witwatersrand of the Orange Free State give 207 Pb/ 206 Pb ages of ca. 3000 Ma. These data wh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63f6bae33c233f94712293450dd97d4c
https://doi.org/10.1098/rsta.1977.0132
https://doi.org/10.1098/rsta.1977.0132
Autor:
C. C. Rundle, M. T. Styles
Publikováno v:
Journal of the Geological Society. 141:15-19
An acid vein from a borehole in the Kennack Gneiss has given a whole-rock Rb-Sr isochron age of 369 ± 12 Ma. This is interpreted as a metamorphic age recording the time of emplacement of the Lizard Complex. This emplacement in late Devonian times wa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6777bebe7d64bfb68cf9658d9c7fe3ea
https://doi.org/10.1144/gsjgs.141.1.0015
https://doi.org/10.1144/gsjgs.141.1.0015
Autor:
C. C. Rundle
Publikováno v:
Journal of the Geological Society. 136:29-38
Rb–Sr whole rock isochron and K–Ar whole-rock and mineral ages suggest that there were four intrusive episodes in the Lake District in Ordovician times, in addition to the widely recognized end-Silurian event. The Carrock Fell Gabbro has given an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c10906d6e35e72e079bea674b3d632c
https://doi.org/10.1144/gsjgs.136.1.0029
https://doi.org/10.1144/gsjgs.136.1.0029