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THE STRUCTURE AND TECTONIC EVOLUTION OF THE JERSEY SHALE FORMATION, ST-OUEN'S BAY, JERSEY, CHANNEL ISLANDS = EVOLUTION STRUCTURALE ET TECTONIQUE DE LA FORMATION SHALE JERSEY, BAIE SAINT-OUEN, JERSEY, ILES ANGLO-NORMANDESHELM DG.1983; PROCEEDINGS OF THE GEOLOGIST'S ASSOCIATION; ISSN 0016-7878; GBR; DA. 1983; VOL. 94; NO 3; PP. 201-216; BIBL. 23 REF.; ILL.Article

MICROSCOPIC AND MEGASCOPIC FABRICS IN THE SKIDDAW GROUP, BLACK COMBE INLIER, ENGLISH LAKE DISTRICT.HELM DG.1969; GEOL. MAG.; GBR; 1969(12), VOL. 106, NUM. 0006, P. 587 A 594Miscellaneous

A METHOD OF ANALYSIS OF INTERSECTING CRENULATION CLEAVAGES IN POLYPHASE DEFORMED MONOTONOUS FORMATIONS = METHODE D'ANALYSE DES CLIVAGES A CRENULATIONS S'ENTRECROISANT DANS DES FORMATIONS MONOTONES DEFORMEES EN PLUSIEURS PHASESHELM DG; SIDDANS AWB.1981; TECTONOPHYSICS; ISSN 0040-1951; USA; DA. 1981-08-01; VOL. 77; NO 1-2; PP. T13-T18; BIBL. 8 REF.; 1 TAB. ; ILL.Article

A RE-INTERPRETATION OF THE ORIGIN OF SANDS AND GRAVELS AROUND BANC-Y-WARREN, NEAR CARDIGAN, WEST WALES.HELM DG; ROBERTS B.1975; GEOL. J.; G.B.; 1975, VOL. 10, NUM. 0002, P. 131 A 146Serial Issue

SKIDDAW SLATES AND THE BORROWDALE VOLCANICS.WADGE AJ; HELM DG; ROBERTS B et al.1971; NATURE PHYS. SCI.; 1971, VOL. 234Miscellaneous

RELATIONSHIP BETWEEN THE SKIDDAW SLATES AND THE BORROWDALE VOLCANICS.JEANS PJF; HELM DG; ROBERTS B et al.1971; NATURE PHYS. SCI.; 1971, VOL. 234, NUM. 0046, P. 59 A 60Miscellaneous

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