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Garin Formation

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Journal Article
Journal: GSA Bulletin
Published: 01 January 2009
GSA Bulletin (2009) 121 (1-2): 17–38.
...) that crosscut an accretionary mélange; and (2) investigating the provenance of clasts in the Garin Formation, the lowermost post-Taconian sedimentary unit. These data allow us to propose a revised geological scenario, using Newfoundland's geology as a template, for this part of the Québec Appalachian orogen...
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Journal Article
Published: 27 April 2004
Canadian Journal of Earth Sciences (2004) 41 (5): 553–570.
...Michel Malo Abstract The Matapédia basin consists of the uppermost Ordovician – lowermost Silurian deep-water, fine-grained carbonate–siliciclastic rocks of the Honorat (Garin Formation) and Matapédia groups (Pabos and White Head formations), the lower rock assemblage of the Gaspé Belt in the Gaspé...
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Journal Article
Published: 01 October 1988
Canadian Journal of Earth Sciences (1988) 25 (10): 1618–1628.
...John Riva; Michel Malo Abstract The Honorat Group of southern Gaspé consists of two formations: the Arsenault and the Garin. The Arsenault Formation, heretofore considered barren, has yielded a graptolite faunule indicative of a Llanvirn–Llandeilo age (early Middle Ordovician), suggesting...
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Outcrop belt of the Arsenault, Cloridorme, Deslandes and <b>Garin</b> <b>Formations</b>, ...
Published: 01 March 2000
Fig. 1. Outcrop belt of the Arsenault, Cloridorme, Deslandes and Garin Formations, eastern Gaspé Peninsula, palinspastically restored after Malo et al. (1992, 1995). Upper right inset shows location of main figure (horizontally hachured area), approximate position of the Popelogan arc (PA
Journal Article
Published: 01 March 2000
Journal of the Geological Society (2000) 157 (2): 393–400.
...Fig. 1. Outcrop belt of the Arsenault, Cloridorme, Deslandes and Garin Formations, eastern Gaspé Peninsula, palinspastically restored after Malo et al. (1992, 1995). Upper right inset shows location of main figure (horizontally hachured area), approximate position of the Popelogan arc (PA...
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U-Pb zircon concordia diagrams for new age determinations from igneous clas...
Published: 01 January 2009
Figure 10. U-Pb zircon concordia diagrams for new age determinations from igneous clasts of the Garin Formation: (A) monzonite RJ-27, and (B) porphyritic rhyodacite/dacite RLH-87.
Image
Generalized composite measured sections of the Deslandes and Cloridorme For...
Published: 01 March 2000
Fig. 2. Generalized composite measured sections of the Deslandes and Cloridorme Formations and the Garin Formation. Stratigraphic positions of individual measured sections for the Deslandes and Cloridorme Formations are shown to the left of the column; see Fig. 1 for locations. Palaeocurrent
Journal Article
Published: 01 June 1988
Canadian Journal of Earth Sciences (1988) 25 (6): 893–908.
... two formations. The Honorat is herein divided into two new formations, the Arsenault and the Garin, which are defined for the first time. The Matapédia Group includes the Pabos and White Head formations. The Pabos Formation, a transitional unit between the noncalcareous strata of the Honorat Group...
Series: Geological Society, London, Special Publications
Published: 09 July 2021
DOI: 10.1144/SP502-2019-151
EISBN: 9781786209900
... dating of the South Maradi PAP formations. Four samples were dated by K–Ar on a MI-1201 IG mass spectrometer and two of them were re-dated by U–Pb on a inductively coupled plasma mass spectrometer. The Dan Issa porphyritic gneiss indicated two weighted average U–Pb zircon ages: 638.3 ± 3.0 Ma (MSWD = 5.4...
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Journal Article
Journal: PALAIOS
Published: 01 November 2010
PALAIOS (2010) 25 (11): 721–729.
... reef complex from Cape Ghir, Morocco (locality 8) belongs to the Lalla Oujja Formation and may include the lowermost Kimmeridgian. Its coral diversity corresponds to the reef climax phase ( Martin-Garin et al., 2007a ). Figure 3. Coral diversity, field sampling methods, and locations...
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Figure 2. Chronostratigraphic position of the three successive Oxfordian co...
Published: 01 November 2010
), Günsberg Member. The coral reef complex from Cape Ghir, Morocco (locality 8) belongs to the Lalla Oujja Formation and may include the lowermost Kimmeridgian. Its coral diversity corresponds to the reef climax phase ( Martin-Garin et al., 2007a ).
Journal Article
Journal: GSA Bulletin
Published: 01 September 2004
GSA Bulletin (2004) 116 (9-10): 1074–1086.
...-Garin and/or Grand-Pabos Faults in the southern Gaspé Peninsula (Fig. 1) . The coarse Saint-Jules Formation detritus in the Paspébiac graben is exclusively composed of sedimentary rock clasts of the Chaleurs Group and was probably derived from closer sources, as these rocks are mainly exposed...
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Journal Article
Journal: Economic Geology
Published: 01 September 2000
Economic Geology (2000) 95 (6): 1297–1318.
... of the Aroostook-Percé anticlinorium disconformably overlies rocks of the Dunnage zone cropping out along the Grand Pabos fault ( Figs. 2 , 3 ). The three overlying formations constitute a conformable sequence of terrigenous rocks (Garin) passing gradually upward to silty and shaly limestones (White Head...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2000
GSA Bulletin (2000) 112 (1): 4–20.
... the Caradocian Nemagraptus gracilis zone to Llandoverian C3, a time interval that roughly corresponds to the Honorat-Matapédia Group age. The Honorat Group (Garin Formation) is conformably overlain by the Pabos and the White Head Formations of the Matapédia Group ( Malo, 1979 , 1986 ; Vennat, 1979...
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Journal Article
Published: 01 February 2009
Russ. Geol. Geophys. (2009) 50 (2): 87–95.
...), formation of solid solutions (incorporation of metal ions into the crystal lattice with substitution of structural cations), and coprecipitation of trace components as secondary phases differing in properties from ordinary bulk phases of the same composition ( Lakshtanov and Stipp, 2007 ; Martin-Garin et...
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Journal Article
Published: 01 April 1999
Journal of the Geological Society (1999) 156 (2): 345–355.
.... Pressure water in the Chad Formation of Bornu and Dikwa emirates, north-eastern Nigeria. Geological Survey of Nigeria. Bulletin 35. Bromley J. Edmunds W.M. Fellman E. Brouwer J. Gaze S.R. Sudlow J. Taupin J.-D. Rainfall inputs and direct recharge to the deep unsaturated...
Journal Article
Journal: Geology
Published: 30 July 2021
Geology (2021) 49 (12): 1431–1435.
... interpretation for horizon DU formation relies on indirect evidence. The thermally controlled subsidence rate for this part of the Mascarene Plateau was ∼0.1 m k.y. −1 for the past 7 m.y. ( Coffin, 1992 ) ( Fig. 1B ). Assuming that horizon DU traces the pre-drowning top of the shallow-water carbonate platform...
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Journal Article
Published: 18 May 2004
Canadian Journal of Earth Sciences (2004) 41 (5): 527–551.
... with the Vauréal Formation on Anticosti Island and with the lower part of the White Head Formation at Percé ( Martin 1980 ; Achab 1989 ). In contrast, the age of correlative rocks of the Garin Formation in the Gaspé Peninsula ranges into the Caradocian, suggesting regional diachroneity in the transition from...
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Journal Article
Published: 18 October 2002
Canadian Journal of Earth Sciences (2002) 39 (10): 1541–1551.
... unconformably on Ordovician mudstones of the Garin and Pabos formations ( Gosselin 1988 ). The Saint-Jules Formation is absent on the Black Cape Ridge, but remnants of the Bonaventure Formation and underlying groundwater calcrete are found on this topographic high, resting unconformably on Silurian rocks...
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Journal Article
Published: 01 October 2005
Mineralogical Magazine (2005) 69 (5): 563–575.
... technologies and consideration of long term hazard ( Young et al. , 2000 ). The literature pertaining to Cd sorption on a wide range of phases is extensive (e.g. Farquhar et al. , 1997 ; Hirsch et al. , 1989 ; Jeanjean et al. , 1995 ; Martin-Garin et al. , 2003 ; Middleburg and Comans, 1991...
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