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Titlebook: Later Proterozoic Stratigraphy of the Northern Atlantic Regions; J. A. Winchester (Lecturer in Geology) Book 1988 Springer Science+Busines

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31#
發(fā)表于 2025-3-27 00:57:23 | 只看該作者
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發(fā)表于 2025-3-27 05:04:19 | 只看該作者
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發(fā)表于 2025-3-27 11:15:00 | 只看該作者
M. Bentleydream scholarship. With contributors working across the disciplines of psychology, history, literature, and cultural studies, it highlights continuities and ruptures in the history of scientific inquiry into dreams..978-3-030-16532-1978-3-030-16530-7Series ISSN 2730-972X Series E-ISSN 2730-9738
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發(fā)表于 2025-3-27 20:11:58 | 只看該作者
J. A. Winchester,B. W. Glovere made and shared theirreligion through experience in history.?This book understands experience as a simultaneously socially constructed and intimately personal process that connects individuals to communities and past to future, thereby forming structures that create and direct societies. It repres
37#
發(fā)表于 2025-3-27 23:16:18 | 只看該作者
Sedimentary structures and sequences within a late Proterozoic tidal shelf deposit: the Upper Morar llow-marine deposits (Long, 1978). Prior to the appearance of stabilizing vegetation during the Palaeozoic, sandy fluvial systems could have adopted an unconfined sheet-braided style, depositing laterally extensive cross-bedded sheet sands (Schumm, 1968; Cotter, 1978). Geometrically similar sand bed
38#
發(fā)表于 2025-3-28 03:55:14 | 只看該作者
The Glenfinnan and Loch Eil Divisions of the Moine Assemblagequently reworked by Caledonian thrusts and related folds at .. 470–420 Ma (Brook .., 1976, 1977; Brewer .., 1979; Powell .., 1981, 1983; Sanders .., 1984; Barr ..,1985). They have an unconformable relationship with late Archaean Lewisian basement granulites and gneisses which are incorporated within
39#
發(fā)表于 2025-3-28 09:41:07 | 只看該作者
40#
發(fā)表于 2025-3-28 12:42:01 | 只看該作者
The Moine Assemblage in Sutherlandorth Sutherland coast. The relative lack of research in the region is even more surprising, as the area has been an enduring source of speculation and controversy for over 100 years. Even the age of deposition and primary deformation of the Moine Assemblage in Sutherland—Proterozoic or Phanerozoic h
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