Margie Series

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Journal Article
Published: 01 April 2008
Scottish Journal of Geology (2008) 44 (1): 75–81.
... of the Margie Limestone of the North Esk . Proceedings of the Geological Society of Glasgow , 124/125 , 27 – 32 . CHEN , X. & WANG , Z. 1993 . The base of the Arenig Series in China . Newsletters on Stratigraphy , 29 , 159 – 164 . CHLUDZINSKI , G.P. 1993 . Lower...
Journal Article
Published: 01 November 2010
Scottish Journal of Geology (2010) 46 (2): 113–124.
... with detritus, which, in the absence of reliable fossils, has provided a control on the stratigraphical order, placing the ‘Margie Series’ younger than the dated Dounans limestone. Tanner & Sutherland (2007) see the complex as divided into two groups one of which overlies, and is a continuation...
FIGURES | View All (15)
Journal Article
Journal: Palynology
Published: 02 April 2020
Palynology (2020) 44 (2): 355–368.
FIGURES | View All (5)
<b>Series</b> of diapirs between rafts. (a) Seismic example from the Angolan <b>margi</b>...
Published: 01 November 2004
Figure 12 Series of diapirs between rafts. (a) Seismic example from the Angolan margin compared with a detailed view of an experimental model, at long sedimentation time intervals, producing columnar diapirs. (b) Close view of an experimental model, at short sedimentation time intervals
Journal Article
Published: 01 August 1970
American Mineralogist (1970) 55 (7-8): 1450–1453.
...Elizabeth A. Wood; Francis Birch; Rustum Roy; Harry J. Rose, Jr. Abstract CRYSTALS AND THEIR STRUCTURES. By Arthur P. Cracknell. Pergamon Press, 1969, 242 p., $7.00 (paper). LANDBOLT-BORNSTEIN: NUMERICAL DATA AND FUNCTIONAL RELATIONSHIPS IN SCIENCE AND TECHNOLOGY. NEW SERIES. VOLUME 2, GROUP III...
Series: AAPG Studies in Geology, AAPG Studies in Geology
Published: 01 January 2008
EISBN: 9781629810331
.... This area is more than 100 km (60 mi) basinward of slope and deltaic deposits of the Tyee Formation (Figures 1 and 3 ). A series of road cuts along Highway 20 exposes up to 460 m (1500 ft) of strike section that shows no evidence of channelization (Figure 4). The primary sedimentary facies here...
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Figure 8. Reconstruction of the northeast Laurentian and West Baltica <b>margi</b>...
Published: 01 July 2007
Supergroup; E—Eriboll Formation; F—Fleur de Lys Supergroup; H—Hedmark Group; L—Labrador Group; Z—Zebra Series.
The sequence at the NW side of the Edzell syncline, North Esk, showing the ...
Published: 01 November 2010
Fig. 4 The sequence at the NW side of the Edzell syncline, North Esk, showing the conglomerate with clasts from the underlying rocks followed by ‘Margie Series’ and then the Dalradian rocks to the NW. This shows the Highland Border sequence to young towards the Dalradian.
Journal Article
Published: 01 October 2015
Journal of Paleontology (2015) 89 (3): 465–486.
...Daniel B. Blake; Thomas E. Guensburg Abstract The class Somasteroidea Spencer, 1951 , is basal within the subphylum Asterozoa. Members are most readily recognized by presence of series of rod-like so-called virgal ossicles extending laterally from each ambulacral ossicle. Five somasteroid genera...
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Journal Article
Published: 01 February 1991
Journal of the Geological Society (1991) 148 (1): 205–206.
... fragments of the ophiolite) and older than the Margie Series of Caradoc age (Curry et al. 1984). Thus the main ophiolite of the Highland Border complex is too young to have been part of the Athollian thickening sequence. The Birchy Schist complex can thus only be correlated with the Green Conglomerate...
Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2014
DOI: 10.1144/M39.7
EISBN: 9781862396821
... of the activity occurred in a 15 min period that included five of the six peaks in PDC generation and two Vulcanian explosions. Although powerful, the PDCs generated were not associated with a lateral blast. The likely cause was the piecemeal collapse of a series of large, unstable lobes that had been extruded...
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Journal Article
Journal: Geosphere
Published: 07 June 2019
Geosphere (2019) 15 (4): 1008–1037.
... but Ti8 ≥ 0.5 (siliceous high-magnesium basalts) and rocks with Si8 ≤ 52 but Ti8 < 0.5 (low-Ti basalts). We tested the classification methodologies using ∼100 low-Ti lava suites dating from the present-day back to the Eoarchean. We conclude that, of those classifying as “boninite series,” Izu-Bonin...
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Journal Article
Published: 01 May 1971
Journal of the Geological Society (1971) 127 (3): 247–271.
... with rejuvenation of Oligocene faults. There is no evidence of lateral movement but many of the faults follow ancient Pre-Cambrian trends. On the Sinai peninsula trend-lines show a twofold directional pattern, parallel to the Gulf of Akada and Gulf of Suez respectively. The angle between them suggests a series...
Journal Article
Published: 01 May 2011
Scottish Journal of Geology (2011) 47 (1): 89–93.
...B. J. Bluck The sequence is established by tracing the petrography of the rocks with earliest being the ophiolite extending its sediments to the later so called Margie Series. It is for these reasons that the of part of the Highland Border rocks belonging to the Dalradian sequence of Tanner...
Journal Article
Published: 01 May 2011
Scottish Journal of Geology (2011) 47 (1): 89–93.
... structures, and neither author referred specifically to the Balmaha area. Bluck follows Barrow (1901) , who inferred that the sequence in the North Esk youngs to the NW, based on the assumption that the Green Conglomerate represents a basal conglomerate to the ‘Margie Series’, derived from...
Journal Article
Published: 01 January 1986
Journal of the Geological Society (1986) 143 (1): 193–198.
.... Establishing a valid stratigraphical correlation for such exposures across the breadth of Scotland has always proved a daunting task full of potential pitfalls. Yet references to these rocks, as the Highland Border Series or the Margie Series , are common in treatments of British stratigraphy, although...
Journal Article
Journal: GSA Bulletin
Published: 06 January 2021
GSA Bulletin (2021)
... et al., 2018, 2019). Lava Samples in the Margi Area The Margi area on the northern flank of the ophiolite is a classic locality in the Troodos Figure 2. Geological map of the Margi area, Cyprus, on the north flank of the Troodos ophiolite (modified after Bai- ley et al., 1991). Sample loca- tions...
Series: Geological Society, London, Special Reports
Published: 01 January 2000
DOI: 10.1144/SR24.11
EISBN: 9781862396920
... by the fauna of the Dounans Limestone Formation, near Aberfoyle (Column 82). Ingham et al. (1986) extracted a large silicified trilobite fauna that could best be correlated with the Cassinian Stage of the Canadian Series of the North American succession. This was confirmed by analysis of the conodont fauna...
Series: GSA Special Papers
Published: 27 November 2018
DOI: 10.1130/2018.2535(16)
EISBN: 9780813795355
..., Royal Ontario Museum, and Andrew Johnston, Smithsonian Institution, for photographs, information, and interesting discussions relevant to this paper; Margie Marino, Executive Director of NMMNHS, Jim Greenhouse, Space Science Director of NMMNHS, the New Mexico Museum of Natural History Foundation...
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Journal Article
Published: 01 August 1982
Journal of the Geological Society (1982) 139 (4): 433–450.
... and the Dalradian sedimen- tary basin are considered within this framework. Exposed intermittently along the Highland Boundary is a distinctive metamorphosed igneous and sedimen- tary assemblage which Barrow (1901) termed the Highland Border Series . We re-define these rocks as the Highland Boundary Complex (H.B.C...