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Monadhliath Semipelite

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Journal Article
Published: 01 February 1989
Journal of the Geological Society (1989) 146 (1): 85–96.
... Formation. (350 m), formerly described as the Monadhliath Semipelite (Okonkwo 1985), exhibits marked lateral variation. It was correlated initially with the Monadhliath Semipelite north-west of the Corrieyairack Granodiorite (Fig. 3) because it possesses a higher proportion of semipelite than the Glen Doe...
Journal Article
Published: 01 February 1982
Journal of the Geological Society (1982) 139 (1): 71–84.
... groups are consistently different: the Leven Schists are muscovite-rich, plagioclase-poor semipelites to pelites, whereas the Monadhliath Schists are a typical ‘Moinian’ semipelite, consisting almost entirely of biotite, sodic andesine and quartz. Equally, consistent geochemical differences between...
Journal Article
Published: 01 June 1975
Journal of the Geological Society (1975) 131 (3): 327–328.
... the R. Spean. During field work for a project on the geochemistry of the Leven and Monadhliath schists (Lambert & Holland in preparation) observations were made on the sequence in the R. Leven E of Kinlochleven which imply conclusions different from those of Treagus (1974 fig. 4, P. 539–41...
Journal Article
Published: 01 August 1990
Journal of the Geological Society (1990) 147 (4): 732–734.
... with the Clachaig Formation with which the Monadhliath Semipelite is correlated, are shown to be of shallow water (marine?) origin by the presence of wave ripples, flaser bedding and traction-dominated deposition. Likewise, sedimentological analysis of the underlying formations assigned to the Corrieyairack...
Journal Article
Published: 01 December 1994
Journal of the Geological Society (1994) 151 (6): 971–986.
... major TECTONOTHERMAL EVOLUTION, MONADHLIATH 983 Table 3. Pressure-temperature estimates obtained from the Appin Group pelitic schists and calc-silicate rocks, and Grampian Group semipelitic schists and calc-silicate rocks Sample N Tm,, Tmax Appin Group: pelitic schisrs S82456 18 390 580 S76868 15 450...
Journal Article
Published: 01 February 1980
Journal of the Geological Society (1980) 137 (1): 41–59.
... in which belts of pelitic and semipelitic schists and gneisses were present, some of the pelites containing quartzites, marbles and amphibolites. Fol- lowing the work of Anderson (1948, 1956) the Moi- nian psammites became known as Eilde (elsewhere the Struan) Flags and the pelites as the Monadhliath...
Journal Article
Published: 01 April 1995
Journal of the Geological Society (1995) 152 (2): 391–406.
...B. W. GLOVER; R. M. KEY; F. MAY; G. C. CLARK; E. R. PHILLIPS; B. C. CHACKSFIELD Abstract The Grampian and Appin groups of the southwestern Monadhliath Mountains form the earliest known syn-rift sequences of the Scottish central Highlands. They were likely to have formed in an intracontinental...
Journal Article
Published: 01 December 1999
Journal of the Geological Society (1999) 156 (6): 1163–1173.
...). Westwards (Fig. 1, area 2), they pass laterally into thinly bedded calcsilicate-bearing semipelite and micaceous psammite, locally with graphitic semipelite and quartzite (the Monadhliath Schist and TarV Banded Forma- tion of Winchester & Glover 1988; Key et al. 1997). These mixed units, with a cumulative...
Journal Article
Published: 01 December 1999
Journal of the Geological Society (1999) 156 (6): 1183–1193.
.... The Moinian and Dalradian rocks between Glen Roy and the Monadhliath Mountains, Invemess-shire Transactions of the Royal Society of Edinburgh: Earth Sciences 1956 63 15 36 Ashworth J.R. Harris A. Holland C.H. Leake B.C. Textural and mineralogical evolution of migmatites...
Journal Article
Published: 01 December 1999
Journal of the Geological Society (1999) 156 (6): 1175–1182.
... basins Belt basement unconformities References Anderson J.G.C. The Kinlochlaggan Syncline, southern Inverness-shire Transactions of the Geological Society of Glasgow 1947 21 97 115 Anderson J.G.C. The Moinian and Dalradian rocks between Glen Roy and the Monadhliath...
Journal Article
Published: 01 June 1999
Journal of the Geological Society (1999) 156 (3): 577–589.
... Anderson J.G.C. The Moinian and Dalradian rocks between Glen Roy and the Monadhliath Mountains, Inverness-shire Transactions of the Royal Society of Edinburgh 1956 63 15 36 Anderton R. Sedimentation and tectonics in the Scottish Dalradian Scottish Journal of Geology 1985 21 407...
Journal Article
Published: 01 November 2004
Scottish Journal of Geology (2004) 40 (2): 159–174.
... Buck Pebbly Psammite and Garva Bridge Pebbly Psammite Formations. The Corrieyairack Subgroup is dominated by plagioclase- bearing, micaceous psammite and has thick horizons of pelite (e.g. Coire nan Laogh Semipelite Formation, Monadhliath Semipelite Formation). In contrast, the Glen Buck Pebbly...
FIGURES | View All (6)
Journal Article
Published: 01 February 1998
Journal of the Geological Society (1998) 155 (1): 13–24.
... 1989 146 85 96 Glover B.W. Key R.M. May F. Clark G.C. Phillips E.R. Chackfield B.C. A Neoproterozoic multiphase rift sequence: the Grampian and Appin groups of the southwestern Monadhliath Mountains of Scotland Journal of the Geological Society, London 1995 152...
Journal Article
Published: 01 December 1996
Journal of the Geological Society (1996) 153 (6): 839–852.
.... M. Clark G. C. Phillips E. R. Chacksfield B. C. A Neoproterozoic multi-phase rift sequence: the Grampian and Appin Groups of the southwestern Monadhliath Mountains of Scotland Journal of the Geological Society, London 1995 152 391 406 Hambrey, M. J., Fairchild, I. J...
Journal Article
Published: 01 April 1981
Journal of the Geological Society (1981) 138 (2): 205–209.
..., it incorporated features from both events. Reassessment of this pattern is now due, particularly with regard to the nature of the Monadhliaths metamorphic ‘high’. However, the relocation of metamorphic zones established by the Grampian event suggested by Wells is oversimplified and unconvincing, and his...
Journal Article
Published: 01 December 1999
Journal of the Geological Society (1999) 156 (6): 1195–1204.
... Geological Society London Special Publications Glover B.W. Key R.M. May F. Clark G.C. Phillips E.R. Chacksfield B.C. A Neoproterozoic multi-rift sequence: the Grampian and Appin groups of the southern Monadhliath Mountains, Scotland Journal of the Geological Society, London...
Journal Article
Published: 22 February 2023
Journal of the Geological Society (2023) 180 (2): jgs2022-134.
... is a monotonous succession, 5 km or more in thickness, of centimetre to decimetre thick graded beds of micaceous psammite, semipelite, pelite and minor quartzite. The proportions of these lithologies vary from area to area ( Fig. 3 ) and, in places near the base of the Corrieyairick Subgroup, there are thin...
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Journal Article
Published: 01 September 1997
Journal of the Geological Society (1997) 154 (5): 917–919.
.... Clark G.C. Phillips E.R. Chacksfield B.C. A Neoproterozoic multi-rift sequence: the Grampian and Appin groups of the southwestern Monadhliath Mountains of Scotland Journal of the Geological Society, London 1995 152 391 406 Hambrey M.J. Correlation of Late Proterozoic...
Series: Geological Society, London, Special Reports
Published: 01 January 1994
DOI: 10.1144/SR22.4
EISBN: 9781786202857
... semipelitic formations, the Ruthven ( Highton 1986 ) or the Coire nan Laogh ( Haselock 1982 ) semipelites and the Monadhliath or Ardair semipelites respectively. In Strathnairn the Ruthven Semipelite comprises coarse gneiss previously assigned to the Central Highland Division. The formation, however...
Journal Article
Published: 01 March 2003
Journal of the Geological Society (2003) 160 (2): 231–246.
... Beds ( Goodman & Winchester 1993 ). The sample is from the basal unit known locally as the Sron Beag Schist and comprises a striped quartzose psammite and schistose semipelite with calcareous bands, taken NE of Lochan na Lairige at NN 5921 4113. Analysed zircon grains (82 analyses) range in age...
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