Výsledky vyhledávání - "G E, Caldwell"

The South Kintyre Basin: its role in the stratigraphical and structural evolution of the Firth of Clyde region during the Devonian–Carboniferous transition

Autor: W. G. E. Caldwell, G. M. Young

Publikováno v: Scottish Journal of Geology. 55:141-154

Late Devonian–Early Carboniferous rocks at the southern end of the Kintyre Peninsula closely resemble those of the Kinnesswood and Clyde Sandstone formations in more easterly portions of the Firth of Clyde. For example, a previously unrecognized th

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d9d4622f8577df9f8a16b2b5e6f5421a
https://doi.org/10.1144/sjg2019-001

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W. G. E. Caldwell (Ed.). 1975. The Cretaceous System in the Western Interior of North America. Proceedings of an international symposium held in Saskatoon,May 1973. ix + 666 pp., numerous figs. Special Paper No. 13. Price $18.00 ($14.00 to GAC members)

Autor: null P. F. R.

Publikováno v: Geological Magazine. 114:489-489

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::1259bd7b5ea4cc01c91d97c0eb564f39
https://doi.org/10.1017/s0016756800045441

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The Cumbrae Islands: a structural Rosetta Stone in the western offshore Midland Valley of Scotland

Autor: G. M. Young, W. G. E. Caldwell

Publikováno v: Scottish Journal of Geology. 49:117-132

Synopsis Although modest in size and topographic expression, the Cumbrae islands hold a key to better understanding of the structurally anomalous portion of the Midland Valley of Scotland underlying the Firth of Clyde. Situated beneath the western ed

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::840f4d8255bfa93f9bfcfce61f30c055
https://doi.org/10.1144/sjg2011-462

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Structural controls in the western offshore Midland Valley of Scotland: implications for Late Palaeozoic regional tectonics

Autor: W. G. E. Caldwell, G. M. Young

Publikováno v: Geological Magazine. 150:673-698

New detailed mapping and related field studies, together with re-assessment of prior investigations, have revealed that three groups of faults, orientated broadly NE, N and NW, have been the primary controls on stratigraphical, structural and geomorp

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::fdbb52c42112f73249b649f47a4f671b
https://doi.org/10.1017/s0016756812000878

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Early Carboniferous minor intrusions of the Clyde Plateau: new data from the Cumbrae islands

Autor: W. G. E. Caldwell, Grant M. Young

Publikováno v: Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 102:227-251

The Cumbrae islands are unmatched for study of minor intrusions associated with the Early Carboniferous Clyde Lava Plateau. The transitional to subalkaline rock suite is present in a linear swarm of c. 250 ENE to NE dykes – 82 ‘basaltic’ (basal

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9eb5d577e05de5eea78fd69cb1ef14f9
https://doi.org/10.1017/s1755691011011030

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Early Carboniferous stratigraphy in the Firth of Clyde area: new information from the Isle of Bute

Autor: W. G. E. Caldwell, G. M. Young

Publikováno v: Scottish Journal of Geology. 47:143-156

Synopsis On the Isle of Bute, the Carboniferous Period is represented mainly by volcanic rocks of the Clyde Plateau Volcanic Formation (Visean, mid- to late Holkerian). Although previously considered to lie on rocks of the Upper Old Red Sandstone (Bu

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::bb4703bf6b2598e70612155ed76b230e
https://doi.org/10.1144/0036-9276/01-431

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The Northeast Arran Trough, the Corrie conundrum and the Highland Boundary Fault in the Firth of Clyde, SW Scotland

Autor: G. M. Young, W. G. E. Caldwell

Publikováno v: Geological Magazine. 149:578-589

Two strikingly different successions of Lower Carboniferous (mainly Tournaisian) sedimentary rocks are closely juxtaposed on the NE coast of the island of Arran, SW Scotland. Near the village of Corrie a thin succession (~ 17 m) of Tournaisian rocks

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6112dc6490c3e6f99ce53ed91c592a0c
https://doi.org/10.1017/s0016756811000823

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Stratigraphical context and geochemistry of Tournaisian (pre-Clyde Plateau Volcanic Formation) tuffs, Great Cumbrae, western Midland Valley of Scotland

Autor: G. M. Young, W. G. E. Caldwell

Publikováno v: Scottish Journal of Geology. 47:21-32

Synopsis In the western part of the Midland Valley of Scotland, Carboniferous volcanic activity is considered to have been initiated at c . 335 Ma with extrusion of the first lavas of the Clyde Plateau Volcanic Formation (CPF). On the island of Littl

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::91fcab406dae191079be791af894984e
https://doi.org/10.1144/0036-9276/01-414

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The Early Carboniferous volcanic outliers of Little Cumbrae and south Bute: implications for westward attenuation of the Clyde Lava Plateau

Autor: G. M. Young, W. G. E. Caldwell

Publikováno v: Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 102:59-76

Little Cumbrae and south Bute are the closest outliers of Early Carboniferous Clyde Plateau volcanic rocks to those forming the plateau itself, and the only ones with the potential to reveal how the volcanic succession of the plateau becomes attenuat

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::df4c0a75ec0d92686d0e13c24615bfc8
https://doi.org/10.1017/s1755691011010048

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