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Titlebook: Synthesis of the Caledonian Rocks of Britain; D. J. Fettes,A. L. Harris Book 1986 D.Reidel Publishing Company, Dordrecht, Holland 1986 Cam

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發(fā)表于 2025-3-21 17:41:50 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱Synthesis of the Caledonian Rocks of Britain
編輯D. J. Fettes,A. L. Harris
視頻videohttp://file.papertrans.cn/885/884315/884315.mp4
叢書(shū)名稱Nato Science Series C:
圖書(shū)封面Titlebook: Synthesis of the Caledonian Rocks of Britain;  D. J. Fettes,A. L. Harris Book 1986 D.Reidel Publishing Company, Dordrecht, Holland 1986 Cam
描述The Advanced Science Institute on which this publication is based took the somewhat unusual form of a geological field symposium held during late August 1984. It was designed to demonstrate to experienced earth scientists from the North Atlantic area the full range of geological phenomena encountered in the British Caledonian rocks. The ASl travelled from South Wales to the far northwest of Scotland by the route shown on the map and in doing so examined sedimentary, igneous and metamorphic rocks from Pembrokeshire (Dyfed), Cardigan (Ceridigian), Snowdonia, Anglesey, the English Lake District and the Southern Uplands and Highlands of Scotland. Thus the fifty or so participants in the ASl studied the geological history and major structures of rocks exposed on either side of the supposed Lower Palaeozoic Iapetus Ocean the British sector of which closed to the south of the present Southern Uplands. Wales (1-5) afforded insight into the nature of the late Precambrian basement of England and Wales and the relationship of sedimentary and volcanic cover sequences to this basement. The Ordovician sequence in Wales is a sample of the volcanic rocks typical of a marginal basin, and were exami
出版日期Book 1986
關(guān)鍵詞Cambrian; Ordovician; Paleozoic; Snow; fault; geology; geophysics; history; map; ocean; orogenic belt; orogeny;
版次1
doihttps://doi.org/10.1007/978-94-009-4654-5
isbn_softcover978-94-010-8568-7
isbn_ebook978-94-009-4654-5Series ISSN 1389-2185
issn_series 1389-2185
copyrightD.Reidel Publishing Company, Dordrecht, Holland 1986
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 21:02:46 | 只看該作者
https://doi.org/10.1007/978-94-009-4654-5Cambrian; Ordovician; Paleozoic; Snow; fault; geology; geophysics; history; map; ocean; orogenic belt; orogeny;
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發(fā)表于 2025-3-22 03:09:19 | 只看該作者
978-94-010-8568-7D.Reidel Publishing Company, Dordrecht, Holland 1986
地板
發(fā)表于 2025-3-22 07:26:11 | 只看該作者
5#
發(fā)表于 2025-3-22 12:39:44 | 只看該作者
A Geotraverse through the Caledonides of Wales,This field guide describes critical exposures to illustrate aspects of the late Proterozoic to early Palaeozoic evolution of the marginal basin in Wales; the full route is shown in Figure 2.1.
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發(fā)表于 2025-3-22 14:40:17 | 只看該作者
Some Aspects of Geophysics in the Caledonides of the UK, to use geophysical data to correlate gross structural zones in the Canadian Appalachians with their postulated counterparts in the British Isles (Haworth, 1980; Haworth and Jacobi, 1983; Jacobi and Kristoffersen, 1981; Lefort, 1980).
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發(fā)表于 2025-3-22 18:56:13 | 只看該作者
The Caledonian Geology of the Scottish Highlands,y, lies a thick sequence of dominantly Devonian and Carboniferous sediments and associated intrusives while to the NW of the Moine Thrust zone are late-Archaean to Middle Proterozoic Lewisian gneisses and granulites, which are overlain by clastic and carbonate sequences of varying age from late Middle Proterozoic to Lower Ordovician age.
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發(fā)表于 2025-3-23 06:23:45 | 只看該作者
The Caledonian Geology of the Scottish Highlands,mited to the SE by the Highland Boundary fault and to the NW by the Moine Thrust zone. Many geologists would now divide the Moine into two (the ‘o1d’ and the ‘Young’) on the basis of radiometric age and structural and metamorphic history. ‘O1d’ Moine rocks have suffered the tectonothermal effects of
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