DOCSLIB.ORG

Download a Pdf Version

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Download a Pdf Version Atlantic Geology 201 Alleghanian faulting in the southern Gaspé Peninsula of Quebec P. Jutras,1 G. Prichonnet,2 and S. McCutcheon3 1. Department of Geology, Saint Mary’s University, Halifax, NS B3H 3C3 <[email protected]> 2. GEOTERAP, Département des Sciences de la Terre et de l’Atmosphère, Université du Québec à Montréal, C.P. 8888, Succ. Centre-ville, Montréal, QC H3C 3P8 3. New Brunswick Department of Natural Resources, P.O. Box 50, Bathurst, NB E2A 3Z1 Date received: July 11, 2003 ¶ Date accepted: January 7, 2004 ABSTRACT Transcurrent faults and associated compressional structures affecting post-Middle Devonian rocks are recognized for the first time in the southern Gaspé Peninsula (Quebec). This region was previously thought to have experienced only minor normal fault readjustments after the Middle Devonian Acadian Orogeny. Four SW-striking fault systems with post-Acadian sinistral motion that have been identified along the north shore of Chaleur Bay are described here. These faults are kinematically compatible with large NW-striking dextral faults in eastern Gaspé, and suggest that these struc- tures reflect a widespread Alleghanian paleostress system that probably affected the entire Quebec Appalachians. RÉSUMÉ Des failles de décrochement et les structures compressives qui leur sont associées affectent des roches post-Dévonien moyen dans le sud de la Gaspésie (Québec) et sont reconnues pour la première fois. Cette région était auparavant considérée comme n’ayant connu que des réajustements mineurs de failles normales après l’orogenèse Acadienne (Dévonien moyen). Quatre systèmes de failles orientées SW-NE ont connus des déplacements senestres post-acadiens et sont analysés dans cet article. Ces failles sont compatibles avec de grands décrochements dextres orientés NW-SE dans l’est de la Gaspésie et suggèrent que ces structures sont associées à des paléostress alléghaniens ayant possiblement affecté les Appalaches québécoises dans leur totalité. INTRODUCTION GEOLOGICAL SETTING Following identification of post-Acadian (post-Middle Pre-Carboniferous rocks in southern Gaspé range in age Devonian) paleostress indicators in the Quebec Appalachians from Neoproterozoic to Early Devonian (Brisebois et al. 1992). by Faure et al. (1996), significant Alleghanian deformation was Upper Neoproterozoic to Cambrian metasedimentary and vol- recently reported in the eastern Gaspé Peninsula near the town canic rocks of the Maquereau Group were first deformed by of Percé (Jutras et al. 2003) (Fig. 1, inset). The present paper the Late Cambrian to Early Ordovician Gaspesian Orogeny reveals that transcurrent and associated compressive struc- (Ayrton 1967). Middle Ordovician sandstone and mudrock tures also affected the narrow belt of Carboniferous rocks that of the Mictaw Group were first deformed by the Middle is exposed on the northern shore of Chaleur Bay, in southern Ordovician Taconian Orogeny, which for most authors Gaspé (Fig. 1). The eastern Gaspé structures are dextral faults includes the Late Cambrian to Early Ordovician Gaspesian striking NW to NNW, but the southern Gaspé structures dis- deformation as an early phase of the Taconian Orogeny cussed herein sinistral faults striking NE (Figs. 2 and 3). (Rodgers 1967; St-Julien and Hubert 1975; de Broucker 1987). This paper provides a structural analysis of faults affecting Upper Ordovician to Lower Devonian sedimentary rocks of the Carboniferous rocks in southern Gaspé, which contains the Honorat, Matapedia and Chaleurs groups, as well as volcanic northwesternmost rock exposures of the composite Upper rocks of the latter group, were first deformed by the Early to Devonian to Permian Maritimes Basin (Fig. 1; inset). The fault Middle Devonian Acadian Orogeny (Malo and Béland 1989; traces tend to form well defined scarps because of the juxta- Malo et al. 1992, 1995; Malo and Kirkwood 1995; Bourque et position of poorly-indurated post-Acadian rocks with more al. 2000; Kirkwood et al. 1995) (Figs. 2 and 3). resistant pre- and syn-Acadian rocks. Hence, some geomorphic The post-Acadian succession in southern Gaspé starts with descriptions are included, as they help to delineate the faults. the Frasnian Miguasha Group (Brideaux and Radforth 1970; Atlantic Geology 39, 201–211 (2003) 0843-5561|03|03201-11$2.65|o 202 P. Jutras et al. Atlantic Geology 203 Fig. 1 Simplified geology of the southern Gaspé Peninsula (modified from Briseboiset al. 1992) showing only post-Acadian rela- tionships, with map areas of figures 2 and 3 outlined. Inset is modified from Giblinget al. (1992). Hesse and Sawh 1992; Prichonnet et al. 1996), which was gently Carleton area (Fig.2) have been attributed to a ~600 m nor- deformed prior to deposition of the Late Devonian to Early mal splay of that fault system (Bernard and St-Julien 1986), Mississippian Saint-Jules Formation (Jutras and Prichonnet although no kinematic indicators were documented. Gosselin 2002) (Fig. 4). The latter occupies approximately the same (1988) also postulated that the Bonaventure Formation was stratigraphic position as the Fountain Lake Group of Nova affected by a normal splay of the Grande-Cascapédia Fault Scotia and is also lithologically similar. (Fig. 2) on account of its anomalously steep dip adjacent to the The overlying fanglomerates of the La Coulée Formation of associated fault scarp (Fig. 5). eastern Gaspé (Jutras et al. 1999), which are stratigraphically Gosselin (1988) considered the converging Petit-Montréal, constrained to the Viséan (Jutras et al. 2001), have not been Mont-St-Joseph and Grande-Cascapédia faults (Grande- recognized in southern Gaspé. However, the groundwater cal- Cascapédia fault system) as steeply dipping late Acadian cretization event that is contemporaneous with this formation reverse faults that were active subsequent to regional Acadian affected the southern Gaspé area as well, above the Saint-Jules folding, but also reports evidence for sinistral and, to a lesser Formation and unconformably below the Viséan Bonaventure degree, dextral movement along subordinate structures of the Formation (Jutras et al. 1999, 2001; Jutras and Prichonnet deformation corridor. The possibility that the present disposi- 2002) (Fig. 4). The calcrete locally digested a karstified regolith tion of the Mississippian strata could have been related to that developed in the upper beds of the Saint-Jules Formation, sug- reverse splay, rather than to a subsequent normal splay, has gesting that a significant hiatus separates the Saint-Jules and La never been evaluated. Coulée formations (Jutras and Prichonnet 2002) (Fig. 4). Near Carleton (Fig. 2), the measured dips of Mississippian The youngest sedimentary rock unit in southern Gaspé is beds increase from east to west in the proximity of the Grande- the early Namurian Pointe Sawyer Formation (Fig. 4), which Cascapédia fault system, until they become slightly overturned has very limited exposure (Fig. 3) and which disconformably (Fig. 6a). The strikes of these beds rotate counter-clockwise overlies the Bonaventure Formation. This unit was correlated along with the dip increase (Fig. 2a). with the early Namurian Mabou Group of Nova Scotia on the The subvertically tilted Mississippian beds that are exposed basis of spore-age and lithological similarities (Jutras et al. near the Grande-Cascapédia fault system at Carleton, which is 2001) (Fig. 4). not exposed at its contact with Mississippian rocks, are affected The entire post-Acadian succession of eastern Gaspé, up to by brittle fault planes (n=5) striking NNE plastered with sinis- the Namurian Chemin-des-Pêcheurs Formation (Jutras et al. tral slickensided calcite fibers (Figs. 6b and 2, stereonet 1; Table 2001), which is not exposed in southern Gaspé, was affected by 1). One WNW-striking dextral fault plane with a similar fabric compressive deformation and kilometric strike-slip displace- was also identified (Fig. 2, stereonet 1; Table 1). Moreover, ments (Jutras et al. 2003). Four additional strike-slip fault cor- two minor east-striking reverse fault planes plastered with ridors recognized in the post-Acadian succession of southern calcite slickenfibers were identified in Mississippian rocks of Gaspé are described below. the nearby Saint-Jules-de-Cascapédia quarry (Fig. 2, stereonet 2; Table 1). The described structures are incompatible with the normal THE GRANDE-CASCAPÉDIA fault hypothesis formulated by previous authors (Bernard and FAULT SYSTEM St-Julien 1986; Gosselin 1988). However, they are compatible with sinistral movement along the Grande-Cascapédia fault Steeply dipping strata of the Bonaventure Formation system, with the sinistral and dextral shears (Fig. 2, stereonet along the Petit-Montréal and Mont-Saint-Joseph faults in the 1) being interpreted as, respectively, R and R’ synthetic Riedel 202 P. JutrasP. et al. et Atlantic Geology Fig. 2 Geology of the southwestern Gaspé Peninsula (modified from Jutras and Prichonnet 2002), together with orientations of fault planes (great circles) and slick- enfibers (dots and dotted arrows) in (1) vertically uplifted Mississippian strata near the Grande-Cascapédia fault system, (2) groundwater calcrete of the Saint-Jules quarry, and (3, 4, 5, and 6) the Black Cape Volcanics. Mapping of pre-Mississippian units was by Bourque and Lachambre (1980) and Gosselin (1988). Inset a: sketch of 203 the drag fold near Carleton. Inset b: enlargement of the Black Cape area. Inset c: interpretation of the subsidiary structures of the Black Cape Fault (bold axis). 204 P. Jutras et al. Atlantic
Load more

Recommended publications
  • The La Coulee Formation, a New Post-Acadian Continental Clastic Unit Bearing Groundwater Calcretes, Gaspe Peninsula, Quebec
    Document generated on 09/23/2021 3:19 p.m. Atlantic Geology The La Coulee Formation, a new post-Acadian continental clastic unit bearing groundwater calcretes, Gaspe Peninsula, Quebec Pierre Jutras, Gilbert Prichonnet and Peter H. von Bitter Volume 35, Number 2, 1999 Article abstract A I km2 erosional remnant of the La Coulee Formation, a previously URI: https://id.erudit.org/iderudit/ageo35_2art03 unrecognized stratigraphic unit, has been studied in the Perce area of the Gaspd Peninsula. It unconformably overlies folded Cambrian to Devonian See table of contents rocks and is unconformably overlain by the mid-Carboniferous Bonaventure Fonnation. The erosional remnant includes the lowest 60 m of this newly identified formation of unknown thickness. Original sedimentary fades are Publisher(s) limited to 50 m of breccia debris flows passing stratigraphically upward into 10m of conglomeratic debris flows. Groundwater calcrete formation has Atlantic Geoscience Society partially or completely transformed the lowest 30 m of the sequence. The depositional environment is interpreted as being related to a proximal ISSN continental alluvial fan. The nearby presence of a saline body of water is inferred to account for thick and massive groundwater calcrete formation and 0843-5561 (print) water-saturated debris flows in a relatively arid climatic context Most of the 1718-7885 (digital) formation was eroded prior to deposition of the Bonaventure Formation. However, the basal groundwater calcretes were more widely preserved. They Explore this journal underlie the Bonaventure Formation in most of the Perce1 area and in the Saint-Elzear area, close to a hundred kilometres to the southwest. Post-sedimentary faulting has affected both the La Coulee and Bonaventure Cite this article formations.
    [Show full text]
  • Fossil Crinoids from the Basal West Point Formation (Silurian), Southeastern Gaspé Peninsula, Québec, Eastern Canada Stephen K
    Document généré le 1 oct. 2021 14:43 Atlantic Geology Fossil crinoids from the basal West Point Formation (Silurian), southeastern Gaspé Peninsula, Québec, eastern Canada Stephen K. Donovan et David G. Keighley Volume 52, 2016 Résumé de l'article Les strates du Silurien au Canada atlantique et dans le sud du Québec URI : https://id.erudit.org/iderudit/ageo52art08 renferment à divers endroits des fossiles de crinoïdes communs, bien qu’il s’agisse de vestiges morcelés. Parmi les nouveaux crinoïdes de la formation de Aller au sommaire du numéro West Point du groupe de Chaleurs (du Ludlow au Pridoli?; Silurien supérieur) de la péninsule de Gaspé, on compte Iocrinus? maennili (Yeltysheva) [observé par ailleurs dans l’étage Katien de l’Estonie], Bystrowicrinus (col.) depressus sp. Éditeur(s) nov. et Cyclocyclicus (col.) sp. aff. C. (col.) echinus Donovan. D’après sa morphologie générale et sa position stratigraphique, il est peu probable Atlantic Geoscience Society qu’Iocrinus? maennili fasse partie de la famille Iocrinidae (ordre Disparida), une famille disparue à la fin de l’Ordovicien. Son nom commun a été jusqu’à ISSN présent épelé incorrectement männili, mannili ou mjannili. La plupart des spécimens de Bystrowicrinus (col.) depressus commun ont un aspect 0843-5561 (imprimé) cyclocyclique, car le lumen pentaétoilé se trouve dans un claustrum très 1718-7885 (numérique) profond généralement obstrué par des sédiments; les spécimens libres de sédiments ont un aspect très distinctif. Cyclocyclicus (col.) sp. aff. C. (col.) Découvrir la revue echinus est semblable à une espèce présente dans l’étage Katien du Pays de Galles nordique. Dans son ensemble, cet assemblage fait davantage penser à l’étage Katien (Ordovicien supérieur).
    [Show full text]
  • Fossil Crinoids from the Basal West Point Formation (Silurian), Southeastern Gaspé Peninsula, Québec, Eastern Canada Stephen K
    Document generated on 09/28/2021 2:45 a.m. Atlantic Geology Fossil crinoids from the basal West Point Formation (Silurian), southeastern Gaspé Peninsula, Québec, eastern Canada Stephen K. Donovan and David G. Keighley Volume 52, 2016 Article abstract Silurian strata of Atlantic Canada and southern Québec locally preserve URI: https://id.erudit.org/iderudit/ageo52art08 common fossil crinoids, albeit mostly as disarticulated remains. New crinoids from the Chaleurs Group, West Point Formation (Ludlow to Pridoli?; Upper See table of contents Silurian) of the Gaspé Peninsula include Iocrinus? maennili (Yeltysheva) (otherwise known from the Katian of Estonia), Bystrowicrinus (col.) depressus sp. nov. and Cyclocyclicus (col.) sp. aff. C. (col.) echinus Donovan. On the basis of Publisher(s) both its gross morphology and stratigraphic position, Iocrinus? maennili is unlikely to be an iocrinid disparid, a family that became extinct at the end of Atlantic Geoscience Society the Ordovician. The trivial name has hitherto been erroneously spelled as männili, mannili and mjannili. Most specimens of the common Bystrowicrinus ISSN (col.) depressus appear cyclocyclic because the pentastellate lumen occurs in a deeply sunken claustrum that is commonly occluded by sediment; clean 0843-5561 (print) specimens are highly distinctive. Cyclocyclicus (col.) sp. aff. C. (col.) echinus is 1718-7885 (digital) similar to a species known from the Katian of North Wales. Taken together, this assemblage is more reminiscent of Katian strata (Upper Ordovician). This is Explore this journal problematic given the current mapping of the outcrop as West Point Formation (Upper Silurian), suggesting further stratigraphic studies in the area are required. Cite this article Donovan, S.
    [Show full text]
  • Chlorophyta, Dasycladales) from the Pridolian to Middle Lochkovian Indian Point Formation, New Brunswick, Canada Steve T
    Document generated on 09/25/2021 8:42 a.m. Atlantic Geology Journal of the Atlantic Geoscience Society Revue de la Société Géoscientifique de l'Atlantique Medusaegraptus (Chlorophyta, Dasycladales) from the Pridolian to middle Lochkovian Indian Point Formation, New Brunswick, Canada Steve T. LoDuca, Randall F. Miller and Reginald A. Wilson Volume 49, 2013 Article abstract Carbonaceous compressions from the Pridolian to middle Lochkovian Indian URI: https://id.erudit.org/iderudit/1062310ar Point Formation in the Flatlands area of New Brunswick comprising a central DOI: https://doi.org/10.4138/atlgeol.2013.005 axis with irregularly arranged unbranched appendages are assigned to Medusaegraptusmirabilis. This is the first report of intact thalli of this See table of contents noncalcified macroalgal taxon from a locality outside of western New York. The biotic composition, stratigraphic context, and sedimentology of this occurrence suggest a shallow-marine depositional setting roughly comparable Publisher(s) to that for the type material of Medusaegraptus mirabilis from Gasport, New York.RÉSUMÉRÉSUMÉLes fossiles carbonés comprimés de la formation Atlantic Geoscience Society d’Indian Point, située dans la région de Flatlands du Nouveau-Brunswick et qui date du Pridolien au Lochkovien moyen, sont attribués àMedusaegraptus ISSN mirabilis; ils présentent un axe central avec des appendices non ramifiés et disposés de façon irrégulière. C’est la première fois qu’on signale la présence 0843-5561 (print) de thalles intacts de ce taxon de macroalgues non calcifiées dans une localité 1718-7885 (digital) ailleurs que dans l’ouest de l’État de New York. La composition biotique, le contexte stratigraphique et les données sédimentologiques permettent de Explore this journal penser à un dépôt marin peu profond à peu près comparable à ce qu’on trouve dans le cas de Medusaegraptus mirabilis de Gasport, dans l’État de New York.[Traduit par la redaction] Cite this article LoDuca, S., Miller, R.
    [Show full text]
  • Restigouche County, New Brunswick
    GAC-MAC-CSPG-CSSS Pre-conference Field Trips A1 Contamination in the South Mountain Batholith and Port Mouton Pluton, southern Nova Scotia HALIFAX Building Bridges—across science, through time, around2005 the world D. Barrie Clarke and Saskia Erdmann A2 Salt tectonics and sedimentation in western Cape Breton Island, Nova Scotia Ian Davison and Chris Jauer A3 Glaciation and landscapes of the Halifax region, Nova Scotia Ralph Stea and John Gosse A4 Structural geology and vein arrays of lode gold deposits, Meguma terrane, Nova Scotia Rick Horne A5 Facies heterogeneity in lacustrine basins: the transtensional Moncton Basin (Mississippian) and extensional Fundy Basin (Triassic-Jurassic), New Brunswick and Nova Scotia David Keighley and David E. Brown A6 Geological setting of intrusion-related gold mineralization in southwestern New Brunswick Kathleen Thorne, Malcolm McLeod, Les Fyffe, and David Lentz A7 The Triassic-Jurassic faunal and floral transition in the Fundy Basin, Nova Scotia Paul Olsen, Jessica Whiteside, and Tim Fedak Post-conference Field Trips B1 Accretion of peri-Gondwanan terranes, northern mainland Nova Scotia Field Trip B8 and southern New Brunswick Sandra Barr, Susan Johnson, Brendan Murphy, Georgia Pe-Piper, David Piper, and Chris White New Brunswick Appalachian transect: B2 The Joggins Cliffs of Nova Scotia: Lyell & Co's "Coal Age Galapagos" J.H. Calder, M.R. Gibling, and M.C. Rygel bedrock and Quaternary geology of the B3 Geology and volcanology of the Jurassic North Mountain Basalt, southern Nova Scotia Dan Kontak, Jarda Dostal, and John Greenough Mount Carleton – Restigouche River area B4 Stratigraphic setting of base-metal deposits in the Bathurst Mining Camp, New Brunswick Steve McCutcheon, Jim Walker, Pierre Bernard, David Lentz, Warna Downey, and Sean McClenaghan Reginald A.
    [Show full text]
  • The Camerate Crinoid Scyphocrinites Zenker in the Upper Silurian Or Lower Devonian of New Brunswick, Canada Stephen K
    Document généré le 27 sept. 2021 12:26 Atlantic Geology Journal of the Atlantic Geoscience Society Revue de la Société Géoscientifique de l'Atlantique The camerate crinoid Scyphocrinites Zenker in the Upper Silurian or Lower Devonian of New Brunswick, Canada Stephen K. Donovan et Randall F. Miller Volume 50, 2014 Résumé de l'article The mid-Paleozoic Scyphocrinites Zenker has a distal attachment modified into URI : https://id.erudit.org/iderudit/1062330ar a globular flotation structure and, uniquely for a crinoid, joined the obligate DOI : https://doi.org/10.4138/atlgeol.2014.014 plankton. Such a flotation structure has been found in the Indian Point Formation (Pridolian to Lochkovian) of Flatlands, northern New Brunswick. It Aller au sommaire du numéro is most likely Pridolian (Upper Silurian) based on the primitive morphology. This identification is confirmed by the globular gross morphology, multi-plated calcite structure, age and similarity to coeval fossils from Cornwall, Éditeur(s) southwestern England. Atlantic Geoscience Society ISSN 0843-5561 (imprimé) 1718-7885 (numérique) Découvrir la revue Citer cet article Donovan, S. & Miller, R. (2014). The camerate crinoid Scyphocrinites Zenker in the Upper Silurian or Lower Devonian of New Brunswick, Canada. Atlantic Geology, 50, 290–296. https://doi.org/10.4138/atlgeol.2014.014 All Rights Reserved ©, 2014 Atlantic Geology Ce document est protégé par la loi sur le droit d’auteur. L’utilisation des services d’Érudit (y compris la reproduction) est assujettie à sa politique d’utilisation que vous pouvez consulter en ligne. https://apropos.erudit.org/fr/usagers/politique-dutilisation/ Cet article est diffusé et préservé par Érudit.
    [Show full text]
  • The Acadian Orogeny: Recent Studies in New England, Maritime Canada, and the Autochthonous Foreland
    Index [Italic page numbers indicate major references] Benner Hill belt, 8,9, 17 accretion, 20, 28, 67, 68, 69, 85 Assemetquagan River area, 111 bentonite beds, 111 Cambrian, 72 Atlantic Realm, 45 Berwick Formation, 11, 52 Caradocian, 72 Atrypa reticularis, 48 Berwick quadrangle, 60 timing, 33 Avalon, 35 Bethlehem pluton, 15 Ackley batholith, 129 Avalon belt, 8, 11,77 Big Berry Mountains syncline, 116 alcids, 42 Avalon block, 19, 78, 80, 126, 130 Bigelow Brook fault complex, 10 Alleghenian Plateau province, 154 Avalon Composite Terrane, 44 Billings Fold, 56 Allegheny County, Maryland, 160 Avalon crust, 11 biogeography allochthons, 136, 148 Avalon island arc, 17 analysis, 43 Allsbury Formation, 75 Avalon superterrane, 9, 11, 12, 13, 14 Cambrian, 41, 44, 47 Alto allochthon, 14 Avalon terrane, 20, 28 Carboniferous, 41, 44, 47 Alton quadrangle, 56, 58, 60 Avalon Zone, 15, 102, 126, 128, 129, bioherms, 109 American Cordillera, 67 130, 148 biostromes, 109 Amity quadrangle, 75 Awantjish Formation, 110 biotite, 58, 129, 139, 146, 148 amphibolites, 9, 106, 129 Aylmer Pluton, 95 Black-Cape Volcanics, 109 andalusites, 63,64, 129 blocks, 20, 35,67, 78, 130, 131 Angers-Dugal Outcrop Belt, 110 backfolds, 64 basement, 78 Angola member, 157 Badger Bay area, 32 continental, 32 Annapolis Valley region, 48 Baie Verte, 130 Blue Hills Nappe, 60 Annieopsquotch Complex, 36 Baie Verte-Brompton Line, 28, 86, 87, Blue Ridge, 14 Anse Cascon Formation, 109 106,117,136 Ansea Pierre-Loiselle Formation, 109 Baie Verte Flexure, 128 Bonaventure Formation, 109 anticlines, 141 Baie Verte Peninsula, 128, 129, 139, Bonnie Bay region, 144 anticlinoria, 8, 51 146 Boston area, 44 Antigonish County, 44, 45 Bailiella, 44 Boston Avalon block, 11 Appalachian basin, 154 Balmoral Group, 118 Boston Basin, 28 autochthonous, 153 Baltic Realm, 44, 47 Boston terrane, 19 Appalachian-Caledonian orogen, 28, faunas, 45 Botwood Group, 32, 34.
    [Show full text]
  • Program and Abstracts
    Atlantic Geoscience Society ABSTRACTS 2004 Colloquium & Annual General Meeting Moncton, New Brunswick The 2004 Colloquium & Annual General Meeting was held at the Delta Beausejour Hotel, Moncton, New Brunswick, on January 30 and 31, 2004. On behalf of the society, we thank Colloquium Chairperson Susan Johnson and her organizing committee (Alan Anderson, Cameron Bartsch, Robin Black, Lori Cook, Russell Hiebert, Ken Howells, Dave Keighley, Maurice Mazerolle, Tansy O'Connor-Parsons, Michael Parkhill, Brian Roulston, Erin Smith, Ian Spooner, Peter Wallace, and Reg Wilson) for providing an excellent meeting. We also wish to acknowledge support of the corporate sponsors: PCS-Potash, New Brunswick Division; McGregor GeoScience Limited; Mineralogical Association of Canada; Corridor Resources Inc.; and the Dean of Science, St. Francis Xavier University. In the following pages, we are pleased to publish the abstracts of oral presentations and posters from the Colloquium, which focused on The First J. Ewart Blanchard Special Session on Geophysics; Environmental Geology; Hydrocarbon Geology; Current Research in the Atlantic Provinces; an Ion Microprobe Workshop; and a tour of the PCS Potash Mine. THE EDITORS Trial This PDF was created using the Free RoboPDF Trial (for evaluation purposes only!) Version Get RoboPDF: An Easy, Affordable Alternative for Creating PDFs - www.robopdf.com Buy RoboPDF Contrasting behaviour of acid-generating rock of the Meguma Supergroup in fresh and salt water Jennifer Arnold, Stephen Armstrong, and Anne Marie O’Beirne-Ryan Department of Earth Sciences, Dalhousie University, Halifax, NS B3H 3J5, Canada Acid rock drainage is a well known problem associated with the Meguma Supergroup in the Halifax region of Nova Scotia, Canada.
    [Show full text]
  • New Mexico's Fossil Record Stuart A
    New Mexico Quarterly Volume 32 | Issue 1 Article 21 1962 New Mexico's Fossil Record Stuart A. Northrop Follow this and additional works at: https://digitalrepository.unm.edu/nmq Recommended Citation Northrop, Stuart A.. "New Mexico's Fossil Record." New Mexico Quarterly 32, 1 (1962). https://digitalrepository.unm.edu/nmq/ vol32/iss1/21 This Contents is brought to you for free and open access by the University of New Mexico Press at UNM Digital Repository. It has been accepted for inclusion in New Mexico Quarterly by an authorized editor of UNM Digital Repository. For more information, please contact [email protected]. Northrop: New Mexico's Fossil Record NEW MEXICO'S FOSSIL-RECORD Published by UNM Digital Repository, 1962 1 New Mexico Quarterly, Vol. 32 [1962], Iss. 1, Art. 21 .. The Eighth Annual U. N. M. Research Lecture The Eighth Annual University of New Mexico Research Lecture was delivered on April 7, 1961, by Dr. Stuart A. Northrop. Now Research Profes­ sor and Curator of the Geology· Museum at the University, Dr. Northrop has served this institution since 1928 as as~istant professor, associate profes­ sor, professor, Chairman of the Department of Geology, Curator of the Geology Museum, and Acting Dean of the Graduate School. Primarily a paleontologist and stratigrapher, he has written several books (including Minerals of New Mexico) and numerous articles on the geology of Gaspe (Quebec), Colorado, and New Mexico. ' . A member of numerous local, state, and national societies, he was presi­ dent, New Mexico Geological Society (1949-50); president, University of New Mexico Chapter of Sigma Xi (1955-56); chairman, Rocky Mountain Section, Ge6logical Society of America (1955-56), and became an Honorary member, New Mexico Geological Society May 4, 1962.
    [Show full text]
  • Index to the Geologic Names of North America
    Index to the Geologic Names of North America GEOLOGICAL SURVEY BULLETIN 1056-B Index to the Geologic Names of North America By DRUID WILSON, GRACE C. KEROHER, and BLANCHE E. HANSEN GEOLOGIC NAMES OF NORTH AMERICA GEOLOGICAL SURVEY BULLETIN 10S6-B Geologic names arranged by age and by area containing type locality. Includes names in Greenland, the West Indies, the Pacific Island possessions of the United States, and the Trust Territory of the Pacific Islands UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.G. - Price 60 cents (paper cover) CONTENTS Page Major stratigraphic and time divisions in use by the U.S. Geological Survey._ iv Introduction______________________________________ 407 Acknowledgments. _--__ _______ _________________________________ 410 Bibliography________________________________________________ 410 Symbols___________________________________ 413 Geologic time and time-stratigraphic (time-rock) units________________ 415 Time terms of nongeographic origin_______________________-______ 415 Cenozoic_________________________________________________ 415 Pleistocene (glacial)______________________________________ 415 Cenozoic (marine)_______________________________________ 418 Eastern North America_______________________________ 418 Western North America__-__-_____----------__-----____ 419 Cenozoic (continental)___________________________________
    [Show full text]
  • The Campbellton Formation, New Brunswick, Canada: a Sedimentological and Paleoenvironmental Description of an Early Devonian (Emsian) Vegetated Landscape
    THE CAMPBELLTON FORMATION, NEW BRUNSWICK, CANADA: A SEDIMENTOLOGICAL AND PALEOENVIRONMENTAL DESCRIPTION OF AN EARLY DEVONIAN (EMSIAN) VEGETATED LANDSCAPE by Kirsten Kennedy Submitted in partial fulfillment of the requirements for the degree of Master of Science at Dalhousie University Halifax, Nova Scotia August 2011 © Copyright by Kirsten Kennedy, 2011 DALHOUSIE UNIVERSITY DEPARTMENT OF EARTH SCIENCES The undersigned hereby certify that they have read and recommend to the Faculty of Graduate Studies for acceptance a thesis entitled ―THE CAMPBELLTON FORMATION, NEW BRUNSWICK, CANADA: A SEDIMENTOLOGICAL AND PALEOENVIRONMENTAL DESCRIPTION OF AN EARLY DEVONIAN (EMSIAN) VEGETATED LANDSCAPE‖ by Kirsten Kennedy in partial fulfillment of the requirements for the degree of Master of Science. Dated: August 17, 2011 Supervisor: ________________________________ Readers: _________________________________ _________________________________ _________________________________ _________________________________ ii DALHOUSIE UNIVERSITY DATE: August 17, 2011 AUTHOR: Kirsten Kennedy TITLE: THE CAMPBELLTON FORMATION, NEW BRUNSWICK, CANADA: A SEDIMENTOLOGICAL AND PALEOENVIRONMENTAL DESCRIPTION OF AN EARLY DEVONIAN (EMSIAN) VEGETATED LANDSCAPE DEPARTMENT OR SCHOOL: Department of Earth Sciences DEGREE: MSc CONVOCATION: October YEAR: 2011 Permission is herewith granted to Dalhousie University to circulate and to have copied for non-commercial purposes, at its discretion, the above title upon the request of individuals or institutions. I understand that my thesis will be electronically available to the public. The author reserves other publication rights, and neither the thesis nor extensive extracts from it may be printed or otherwise reproduced without the author‘s written permission. The author attests that permission has been obtained for the use of any copyrighted material appearing in the thesis (other than the brief excerpts requiring only proper acknowledgement in scholarly writing), and that all such use is clearly acknowledged.
    [Show full text]
  • Hydrothermal Dolomitization in the Lower Silurian La Vieille Formation in Northern New Brunswick: Geological Context and Significance for Hydrocarbon Exploration
    BULLETIN OF CANADIAN PETROLEUM GEOLOGY VOL. 54, NO. 4 (DECEMBER, 2006), P. 380-395 Hydrothermal dolomitization in the Lower Silurian La Vieille Formation in northern New Brunswick: geological context and significance for hydrocarbon exploration DENIS LAVOIE GUOXIANG CHI Geological Survey of Canada Department of Geology Québec Division University of Regina 490 de la Couronne 3737 Wascana Parkway Québec City, QC G1K 9A9 Regina, SK S4S 0A2 ABSTRACT Hydrothermal dolomites are potential hydrocarbon reservoirs in the Late Ordovician–Middle Devonian Gaspé Belt in eastern Canada. These dolomites are recognized in the Lower Silurian Sayabec Formation, Upper Silurian–lowermost Devonian West Point Formation and Lower Devonian Upper Gaspé Limestones and are also recognized in the Lower Silurian La Vieille Formation in northeastern New Brunswick. Hydrothermal dolomitization is expressed in local pervasive dolomitization fronts originating from fracture feeders and by saddle dolomite and high temperature late calcite cements filling fractures and associated dissolution voids. Field evidence such as dolomite clasts in a post-Salinic (early Ludlovian) conglomerate indicates a dolomitization event early in the burial history. Petrographic study documents a complex history of multiple fracture generation and saddle dolomite and/or calcite cement precipitation. Saddle dolomite is locally brecciated and cemented by a later phase of dull luminescent, mm-sized calcite crystals (calcite 1), the latter, in some cases, also completely filling fractures. Saddle dolomite is locally dedolomitized which is expressed as bright luminescent sub-millimetre-sized calcitic zones. Dedolomitization is associated with calcite-cemented (calcite 2), late δ18 stage fractures. OVPDB values of the saddle dolomite (–17.3 to –10‰) and calcite 1 (–13.8 to –8.8‰) cements indicate precipitation from an 18O-depleted fluid and/or at relatively high temperatures.
    [Show full text]