1 edition of Tectonics of southern Nova Scotia found in the catalog.
Tectonics of southern Nova Scotia
J. Duncan Keppie
|Statement||by J. Duncan Keppie.|
|Series||Paper / Province of Nova Scotia, Department of Mines ;, 77-1|
|LC Classifications||QE601 .K37 1977|
|The Physical Object|
|Pagination||34 p. :|
|Number of Pages||34|
|LC Control Number||84199888|
Nova Scotia Dinosaur bones found in Bay of Fundy cliffs Experts find some of Canada's oldest dinosaur bones embedded in red sandstone on the northern shore of Nova Scotia. A Plate Tectonics Flip Book Around million years ago, Pangaea began to break up. The breakup resulted in two landmasses: Laurasia, the northern group of continents, and Gondwanaland, the southern group of continents; Gondwanaland included South America, Antarctica, Australia, Africa, and . Southern Nova Scotia is the only piece of Meguma terrane anywhere on the planet. The Avalon terrane is bigger and very fragmented. Pieces of it are recognized from Connecticut all the way to Newfoundland and across the Atlantic Ocean into the UK and as far as Poland (the Atlantic Ocean didn’t exist yet when the Avalon terrane docked on to the.
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Cover and Table of Contents; Tectonics of Southern Nova Scotia; Acknowledgments; References; Table 1.
Summary of the geological history of southern Nova Tectonics of southern Nova Scotia book. Additional Physical Format: Online version: Keppie, J. Duncan. Tectonics of southern Nova Scotia.
Halifax, Nova Scotia: Province of Nova Scotia, Dept. of Mines, PAPER PLATE TECTONIC INTERPRETATION OF PALAEOZOIC WORLD MAPS (WITH EMPHASIS ON CIRCUM-ATLANTIC OROGENS AND SOUTHERN NOVA SCOTIA). Duncan. Keppie] on *FREE* shipping on qualifying offers. The Meguma Supergroup of Southern Nova Scotia: Insights on Stratigraphy and Tectonic Setting1 C.
White and S. Barr The easternmost tectonic element of the northern Appalachian orogen, the Meguma terrane, includes the Cambrian-Ordovician Goldenville and Halifax formations (Meguma Group) and the younger White Rock.
The Meguma Supergroup of southern Nova Scotia: new insights on stratigraphy, tectonic setting, and provenance Chris E. White,1 Sandra M. Barr,2 John W.F. Tectonics of southern Nova Scotia book Antonio Simonetti,3 and Larry M.
Heaman3 1. Nova Scotia Department of Natural Resources, PO BoxHalifax, NS, Canada B3J 2T9. Department of Geology. The trench-pulling effect of the north dipping subduction, which developed along the new continental margin caused rifting, creating the back-arc basin as well as transfer of plates from Gondwana to Laurasia.
The present authors applied this model to the southern margin of Cited by: changes wrought by plate tectonics. The Cambrian fossils of Nova Scotia are distinctly different from those farther northwest.
To explain this, in a paleogeographic map published in (before the “rebirth” of the continental-drift theory about ), Dunbar inserted a land barrier to separate the Cambrian sea of Nova Scotia from that of New Bruns.
It separates the Meguma Terrane of southern Nova Scotia from the Avalon Terrane to the north. These terranes are distinct tectonic and lithological entities in the Appalachian Orogen. Two areas at either end of this fault system have been examined in detail to determine the sense and history of offset along by: I picked it up because I have family now living on South Mountain in Nova Scotia, and this case from the s brought notoriety to the area.
The book gives an interesting history of the place and of the dissident Puritan families who settled there in the hills in the 18th century, remained insular, and, for generations, poor and poorly educated/5. Southern Nova Scotia or the South Shore is a region of Nova Scotia, area has no formal identity and is variously defined by geographic, county and other political boundaries.
Statistics Canada, defines Southern Nova Scotia as an economic region, composed of Lunenburg County, Queens County, Shelburne County, Yarmouth County, and Digby es: Lunenburg County, Queens. The White Rock Formation in the Yarmouth area of the Meguma terrane of southern Nova Scotia consists mainly of mafic tuffaceous rocks with less abundant mafic flows, epiclastic and clastic sedimentary rocks, and minor intermediate and felsic crystal by: Sandra Barr is a faculty member in the Department of Earth and Environmental Science at Acadia University in Wolfville.
Widely recognized as an expert in the geology of Nova Scotia, she is also co-editor of the scientific journal Atlantic Geology, and is book editor for the Geological Association of Canada.
Martha Hickman Hild has a PhD in Earth Sciences and is a member of the American 4/4(7). The relief and geophysical characteristics of the sea floor in the Drake Passage-Scotia Sea zone have been studied quite well in general.
The oceanic floor within this zone is usually considered as a collage of small fragments of the continental bridge and of young oceanic plates formed by spreading under the large-scale motions of large lithospheric by: 2.
Most of the existing plate tectonic reconstructions (e.g., Klitgord and Schouten, ) show a single salt basin between Nova Scotia and Morocco during the Late Triassic. On the basis of the regional seismic data sets presented in this paper, the Late Triassic to Early Jurassic salt basins of Nova Scotia and Morocco were separated by a regional.
Tectonic deformation and magmatism along the southern flank of the Maritimes Basin: the northeastern Cobequid Highlands, Nova Scotia1 Horton Group Maritime Provinces Eastern Canada faults Paleozoic Maritimes Basin mylonites metamorphic rocks intrusions Nova Scotia lineation metaigneous rocks tectonics structural by: The tectonic evolution of the Nova Scotian passive margin includes a Late Triassic-Early Jurassic rift phase and two major episodes of postrift subsidence spanning Jurassic to early Tertiary time.
The Upper Triassic Chedabucto Formation, Guysborough County, Nova Scotia: depositional and tectonic context Article (PDF Available) in Atlantic Geology 35(2) August with 41 Reads. Sandra Barr is a faculty member in the Department of Earth and Environmental Science at Acadia University in Wolfville.
Widely recognized as an expert in the geology of Nova Scotia, she is also co-editor of the scientific journal Atlantic Geology, and is book /5(7). Jacquelyn E Stevens, J Brendan Murphy and Fred W Chandler, Geochemistry of the Namurian Lismore Formation, northern mainland Nova Scotia: sedimentation and tectonic activity along the southern flank of the Maritimes Basin, Canadian Journal of Earth Sciences, /e, 36.
Introduction  The separation between Greenland and Canada has remained largely unsolved because of an insufficient understanding of the crustal nature in Baffin Bay and Davis Strait and the tectonic relationship of both areas to the Labrador Sea.
In order to address this problem, the German research vessel Maria S. Merian carried out a geophysical survey in Davis Strait and southern Cited by: A revised plate reconstruction of minimum closure (i.e., at final separation), shows similar regional scale transitions along both the Nova Scotian and Moroccan margins.
The southern transition off Nova Scotia occurs at a significant change in the character of the ECMA and the southern. Further paleomagnetic evidence for oroclinal rotation in the central folded Appalachians from the Bloomsburg and the Mauch Chunk Formations Grommé and John W.
Hillhouse, Paleomagnetism of the Resurrection Peninsula, Alaska: Implications for the tectonics of southern Alaska and the Kula Cumberland Structural Basin, Nova Scotia, Journal.
Study of the tectonic development of the Scotia Sea region started with basic lithological and structural studies of outcrop geology in Tierra del Fuego and the Antarctic Peninsula. To nineteenth- and early twentieth-century geologists, the results of these studies suggested the presence of a submerged orocline running around the margins of the Cited by: The southern and southwestern parts of Nova Scotia were regionally metamorphosed during the Devonian Acadian Orogeny (around Ma), when a relatively small continental block (the Meguma Terrane ) was pushed up against the existing eastern margin of North America.
As shown in Figureclastic sedimentary rocks within this terrane were Author: Steven Earle. Pre-Rift. The Scotian Basin is located offshore Nova Scotia where it extends for km from the Yarmouth Arch / United States border in the southwest to the Avalon Uplift on the Grand Banks of Newfoundland in the northeast ().With an average breadth of km, the total area of the basin is approximatelykm of the basin lies on the present-day continental shelf in water depths.
The Scotia Plate is a tectonic plate on the edge of the South Atlantic and Southern Ocean. Thought to have formed during the early Eocene with the opening of the Drake Passage that separates South America from Antarctica, it is a minor plate whose movement is largely controlled by the two major plates that surround it: the South American Plate and Antarctic Plate.
Roughly rhomboid, extending Type: Minor. The Avalon Terrane in Maritime Canada extends from Cape Breton Island through northern Nova Scotia (Antigonish and Cobequid highlands) to southern New Brunswick.
The terrane contains abundant late Proterozoic volcanic rocks (∼– m.y. old).Cited by: Field relationships, petrology, age, and tectonic setting of the Late Cambrian-Ordovician West Barneys River Plutonic Suite, southern Antigonish Highlands, Nova Scotia, CanadaCited by: "The Appalachians constitute one of Earth's major tectonic features and have served as a springboard for innovative geologic thought for more than years.
This volume contains 36 original papers reporting the results of research performed throughout nearly the entire length and breadth of the Appalachian region, including all major provinces and geographical areas. "Lithochemistry of the Lower Paleozoic Goldenville and Halifax groups, southwestern Nova Scotia, Canada: Implications for stratigraphy, provenance, and tectonic setting of the Meguma terrane", From Rodinia to Pangea: The Lithotectonic Record of the Appalachian Region, Richard P.
Tollo, Mervin J. Bartholomew, James P. Hibbard, Paul M. Karabinos. The southern Chile Trench, caused by the subduction of the South American plate, also forms part of the western border.
The eastern edge of the Scotia plate is the East Scotia Ridge, a divergent boundary which is spreading at a rate of 60 mm/yr in the northern part of the East Scotia Ridge to 70 mm/yr in the southern portion. Plate tectonic interpretation of Palaeozoic world maps.
Halifax, N.S.: Province of Nova Scotia, Dept. of Mines, (OCoLC) Material Type: Government publication, State or province government publication: Document Type: Book: All Authors / Contributors: J Duncan Keppie. HISTORY OF NOVA SCOTIA: Book #1, The Lion & The Lily () § A Table of Seven Parts.
HISTORY OF NOVA SCOTIA: Book #2, Settlement, Revolution & War () § A Table of Five Parts. HISTORY OF NOVA SCOTIA: Book #3, The Road To Being Canada () § A Table of Chapters.
NOVA SCOTIAN BIOGRAPHIES () DATE LIST. GLOSSARY. Presents the first reference book to cover salt tectonics of Permo-Triassic period rocks; Features case studies of passive margins like the Barents and the North Sea, Greenland, Nova Scotia, offshore Mauritania, Morocco and Iberia, and folded belts like the Betics-Rif, Tell, Pyrenees, Atlas Mountains, Alps, Balkans, Apennines, the Adriatic and Ionian Seas, and the Zechstein Basin in Norway.
A large part of southern Nova Scotia is made up of granites (South Mountain Batholith) ( million years old) exposed at surface.
What plate tectonic and geological conditions were necessary to produce this large volume of granite. Books shelved as nova-scotia: The Book of Negroes by Lawrence Hill, Fall on Your Knees by Ann-Marie MacDonald, The Birth House by Ami McKay, No Great Mis.
The central Nova Scotia margin off Eastern Canada is located at a transition from a volcanic margin in the south to a non volcanic margin in the north. In order to study this transition, a wide angle refraction seismic line with dense airgun shots was acquired across the central Nova Scotia Cited by: Figure 1: General tectonic features of the Himalaya and southern Tibet 5,8–10,15, Numbers 1–9 correspond to important features requiring explanation 10 Cited by: The Topography of the Sea Floor We examined the topography of the sea floor from the perspective of plate tectonics in Chap but here we are going to take another look at the important features from an oceanographic perspective.
The topography of the northern Atlantic Ocean is shown in Figure Author: Steven Earle. The Antigonish Highlands of northern mainland Nova Scotia and the Mira terrane of southern Cape Breton Island are both part of Avalonia (Fig.
1), characterized by Neoproterozoic volcanic, sedimentary, and plutonic rocks overlain by Cambrian-Ordovician mainly sedimentary rocks (e.g., Hibbard et al. Tectonics (General) Tectonics (General) Nova Scotia’s offshore energy industry is in the global spotlight after an enticing assessment of resources in the Scotian Basin.
some of the key and most spectacular localities of the southern Pyrenees have been selected along the ECORS-Pyrenees transect. This is a reference cross-section. Meanwhile, Dr.
Scotese said, the biggest tectonic change of all — driven by a giant subduction zone — has torn through the dark Atlantic and begun to. Free Online Library: Sedimentary and tectonic setting of a mass-transport slope deposit in the Halifax Group, Halifax Peninsula, Nova Scotia, Canada.(Report) by "Atlantic Geology"; Earth sciences Carbonates Folds (Geology) Natural history Fossils Rocks, Sedimentary Sedimentary rocks Silicates Tectonics Tectonics (Geology).