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{"title":"Classic Rock Tours 3. Grand Canyon Geology, One Hundred and Fifty Years after John Wesley Powell: A Geology Guide for Visiting the South Rim of Grand Canyon National Park","authors":"K. Karlstrom, L. Crossey","doi":"10.12789/geocanj.2019.46.153","DOIUrl":"https://doi.org/10.12789/geocanj.2019.46.153","url":null,"abstract":"The year 2019 is the 150th anniversary of John Wesley Powell’s epic exploration of the Colorado River through Grand Canyon and the 100th anniversary of the establishment of Grand Canyon National Park. This is an excellent moment to look back 150 years to think about where we have come from as a science and society, and look forward 100 years towards the accelerated change we expect in the future. For historians, archaeologists, geologists and astronomers, of course, this century-long time scale is short compared to other perspectives. They might choose also to celebrate the 479th anniversary of the first sighting of Grand Canyon by Europeans in 1540, the 1000th anniversary of Ancestral Puebloan farmers in Grand Canyon, the 12,000th anniversary of the arrival of humans migrating south from the Bering Land Bridge, the 5 millionth anniversary of the integration of the Colorado River through Grand Canyon to the Gulf of California, the 4.6 billionth anniversary of the formation of Earth, or the 13.75 billionth anniversary of the Big Bang and the formation of our Universe. Geology is all about time, and knowing some geology helps with the difficult endeavour of placing human timeframes into perspectives of deep time.  This guide is for geology students of all levels and types visiting the South Rim of Grand Canyon. It is designed as a 3-day field trip and introduction to the rocks and landscapes. The term ‘students’ in our view also includes visitors who want to know about the basics of Grand Canyon geology while taking scenic hikes to see the geology first-hand. It is organized as if you enter the Park at its East entrance, near Cameron, and exit the Park at the South entrance, towards Flagstaff, but the three activities can be done in any order. As an introduction, we present a brief summary of the history of geologic maps and stratigraphic columns, and the geologists who made them. The maps and depictions of Grand Canyon geology over the past 160 years record a visual progression of how geoscience knowledge in general has developed and matured. The first sixty years, before the Park was founded, may have been the greatest in terms of the rapid growth that merged geology, art and public outreach. The second fifty years (to about 1969) saw important advances in stratigraphy and paleontology and solid efforts by the Park to apply and interpret Grand Canyon geology for the public. The most recent 50 years have seen major advances in regional geological mapping, dating of rocks, plate tectonics, and improved geoscience interpretation. The next 100 years will hopefully see additional innovative efforts to use the iconic field laboratory of Grand Canyon rocks and landscapes to resolve global geoscience debates, inform resource sustainability imperatives and contribute to science literacy for an international public.  The three activities described are as follows: Activity 1 (an hour or two) is an overview from Lipan Point. This is a vehicle pull-out on the","PeriodicalId":55106,"journal":{"name":"Geoscience Canada","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-12-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47631472","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The Challenges of Big Data in Expanding Geoscience: Embracing New Initiatives to Untangle our World","authors":"Dène Tarkyth","doi":"10.12789/geocanj.2019.46.152","DOIUrl":"https://doi.org/10.12789/geocanj.2019.46.152","url":null,"abstract":"It was my pleasure to serve as the president of this organization through 2018 and part of 2019, and such an experience cannot help but remind me of the effort that comes from GAC staff and our many volunteers, but it also brought home the challenges that all of us face in organizing our time and activities in this so-called Information Age. We live in a world where both space and time are increasingly compressed, and all of us at times struggle to manage the demands of our work and our lives beyond the office walls. So I will start this address by asking you all to imagine that you had one extra day a week given to you some time that you could spend on fun science and investigating exciting questions, or just catching up on work and life. Would we not all welcome such a gift? But then look back over the last few weeks, months or even years and think about how much time you spent searching for information, skimming papers to finding sample locations, compiling and cleaning up data, georeferencing maps....just some of the many basic things that need to get done before you can get to the fun part of your job as a geoscientist. There are estimates that geologists now spend 80% of their time searching for, formatting and organizing information and data, and I do not find these hard to believe. A recent article highlighted the approach taken by Cameco, one of Canada’s leading mining companies, to change how they manage data in order to save 20% of their geologists’ time – one day a week – so that they would not have to spend countless hours looking for data and could do geology instead (Heffernan 2015). There are many efforts to amalgamate and process data in ways that make this process easier and more amenable to automation. A young student geologist at Princeton University, Julia Wilcots, undertook a summer project with a senior researcher at University of Wisconsin to examine the distribution of stromatolites through geological time by searching descriptive literature. Anyone who has worked in the Precambrian, or indeed in sedimentary rocks of any Eon or Era, can well imagine the immensity of that search. However, through the use of computer search techniques and the ‘Geodeepdive’ database, she was quickly able to identify over 10,000 papers that mentioned stromatolites (in the text, but not necessarily in the title) and extract the associated rock unit names from 10% of them. Then, by linking these results to the ‘Macrostat’ database, she was then able to come up with an estimate of the percentage of shallow marine rocks that contain stromatolites within different geological time periods. A more senior researcher at the University involved with the project estimated that doing this same search would have taken him sixteen months of tedium. The overall conclusions of the study – that the distribution of stromatolites is most closely linked to the abundance of dolomitic carbonate rocks (Peters et al. 2017) – are important, but the methodology demons","PeriodicalId":55106,"journal":{"name":"Geoscience Canada","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-12-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"49488220","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The Rise and Fall of the Dinosaurs: A New History of a Lost World","authors":"T. Rivers","doi":"10.12789/geocanj.2019.46.151","DOIUrl":"https://doi.org/10.12789/geocanj.2019.46.151","url":null,"abstract":"","PeriodicalId":55106,"journal":{"name":"Geoscience Canada","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-10-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46227226","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Great Mining Camps of Canada 7. The Bathurst Mining Camp, New Brunswick, Part 1: Geology and Exploration History","authors":"S. Mccutcheon, J. Walker","doi":"10.12789/geocanj.2019.46.150","DOIUrl":"https://doi.org/10.12789/geocanj.2019.46.150","url":null,"abstract":"The Bathurst Mining Camp of northern New Brunswick is approximately 3800 km2 in area, encompassed by a circle of radius 35 km. It is known worldwide for its volcanogenic massive sulphide deposits, especially for the Brunswick No. 12 Mine, which was in production from 1964 to 2013. The camp was born in October of 1952, with the discovery of the Brunswick No. 6 deposit, and this sparked a staking rush with more hectares claimed in the province than at any time since.   In 1952, little was known about the geology of the Bathurst Mining Camp or the depositional settings of its mineral deposits, because access was poor and the area was largely forest covered. We have learned a lot since that time. The camp was glaciated during the last ice age and various ice-flow directions are reflected on the physiographic map of the area. Despite abundant glacial deposits, we now know that the camp comprises several groups of Ordovician predominantly volcanic rocks, belonging to the Dunnage Zone, which overlie older sedimentary rocks belonging to the Gander Zone. The volcanic rocks formed during rifting of a submarine volcanic arc on the continental margin of Ganderia, ultimately leading to the formation of a Sea of Japan-style basin that is referred to as the Tetagouche-Exploits back-arc basin. The massive sulphide deposits are mostly associated with early-stage, felsic volcanic rocks and formed during the Middle Ordovician upon or near the sea floor by precipitation from metalliferous fluids escaping from submarine hot springs.   The history of mineral exploration in the Bathurst Mining Camp can be divided into six periods: a) pre-1952, b) 1952-1958, c) 1959-1973, d) 1974-1988, and e) 1989-2000, over which time 45 massive sulphide deposits were discovered. Prior to 1952, only one deposit was known, but the efforts of three men, Patrick (Paddy) W. Meahan, Dr. William J. Wright, and Dr. Graham S. MacKenzie, focused attention on the mineral potential of northern New Brunswick, which led to the discovery of the Brunswick No. 6 deposit in October 1952. In the 1950s, 29 deposits were discovered, largely resulting from the application of airborne surveys, followed by ground geophysical methods. From 1959 to 1973, six deposits were discovered, mostly satellite bodies to known deposits. From 1974 to 1988, five deposits were found, largely because of the application of new low-cost analytical and geophysical techniques. From 1989 to 2000, four more deposits were discovered; three were deep drilling targets but one was at surface. \u0000RÉSUMÉLe camp minier de Bathurst, dans le nord du Nouveau-Brunswick, s’étend sur environ 3 800 km2 à l’intérieur d’un cercle de 35 km de rayon. Il est connu dans le monde entier pour ses gisements de sulfures massifs volcanogènes, en particulier pour la mine Brunswick n° 12, exploitée de 1964 à 2013. Le camp est né en octobre 1952 avec la découverte du gisement Brunswick n° 6 et a suscité une ruée au jalonnement sans précédent avec le plus d’hec","PeriodicalId":55106,"journal":{"name":"Geoscience Canada","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-10-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43612822","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Classic Rock Tours 2. Exploring a Famous Ophiolite: A Guide to the Bay of Islands Igneous Complex in Gros Morne National Park, Western Newfoundland, Canada","authors":"A. Kerr","doi":"10.12789/geocanj.2019.46.149","DOIUrl":"https://doi.org/10.12789/geocanj.2019.46.149","url":null,"abstract":"Ophiolites are complex assemblages of ultramafic and mafic igneous rocks that are now widely considered to be pieces of ancient oceanic crust that were emplaced on to the continents courtesy of global plate tectonics. However, most examples were originally considered parts of enormous layered mafic intrusions and so were interpreted in that light. The new understanding of ophiolites in the late 1960s and early 1970s was a crucial part of the global Earth Science revolution, and they are now central to all plate tectonic models developed for ancient orogenic belts. Although their equivalence to oceanic crust is now well established, many ophiolites may not be ‘typical’ examples of such, and not all examples are identical. Most ophiolites likely formed in subduction-influenced environments rather than at mid-ocean ridges. Ophiolites remain important foci for research in the 21st century, and many questions remain about their environments of formation and especially their mechanisms of emplacement onto the continents. Although it was not the first to be seen as a relic of a vanished ocean, the Bay of Islands Igneous Complex in western Newfoundland is one of the best preserved and most easily accessible ophiolites in the world. In the late 20th century, research work in this area proved highly influential in understanding the oceanic crust, and in unravelling the diachronous events involved in the progressive destruction of an ancient stable continental margin as arcs and microcontinental blocks were accreted along it. Parts of the Tablelands Ophiolite lie within Gros Morne National Park, which is a UNESCO world heritage site because of its importance to our understanding of global tectonics. The wider region around the park also includes the Cabox Aspiring Geopark Project, now also in the process of seeking recognition through UNESCO.   This article provides background information on ophiolites and the development of our ideas about them, and links this material to four self-guided field excursions that allow examination of many classic features. These excursions range from a collection of roadside outcrops, to some relatively easy hiking excursions on official National Park trails, and eventually to a more challenging off-trail hike that ascends to the summit plateau of the Tablelands to visit rare exposures of the Moho (the Mohorovičić Discontinuity, i.e. the lower boundary of the Earth’s crust) and the underlying upper mantle rocks. Collectively, the field stops should allow geologically-minded visitors to experience some amazing geology in a spectacular and sometimes surreal landscape. \u0000RÉSUMÉLes ophiolites sont des assemblages complexes de roches ignées ultramafiques et mafiques qui sont maintenant généralement considérées comme des fragments de croûte océanique ancienne qui ont été charriés sur les continents grâce à la tectoniqueglobale des plaques. Cependant, la plupart des exemples étaient à l'origine considérés comme faisant partie de vast","PeriodicalId":55106,"journal":{"name":"Geoscience Canada","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-10-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47731921","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Igneous Rock Associations 24. Near-Earth Asteroid Resources: A Review","authors":"Liam Innis, G. Osinski","doi":"10.12789/GEOCANJ.2019.46.147","DOIUrl":"https://doi.org/10.12789/GEOCANJ.2019.46.147","url":null,"abstract":"The extraction of natural resources located beyond Earth to create products can be described as space resource utilization (SRU). SRU is under active investigation in both the public and private sectors. Near-Earth asteroids (NEAs) are particularly promising early SRU targets due to their relative proximity and enrichments in two key resources: water and platinum group elements (PGEs). Water can be used to create rocket propellant, making it the only resource with significant demand given the current nascent state of the space market. Platinum group elements are valuable enough that their import to the Earth market is potentially economical, making them the other prospective resource in the current embryonic state of SRU. While it is possible to retrieve material from a NEA, doing so on an economical scale will require significant developments in areas such as autonomous robotics and propulsion technology. A parameterization accounting for asteroid size, resource concentration, and accessibility yields just seven and three potentially viable NEA targets in the known population for water and PGEs, respectively. A greater emphasis on spectral observation of asteroids is required to better inform target selection for early prospecting spacecraft. A further complication is the lack of a legal precedent for the sale of extraterrestrial resources. The Outer Space Treaty prohibits the appropriation of celestial bodies but makes no explicit reference to their resources while the U.S.A. and Luxembourg have passed legislation entitling their citizens to own and sell space resources. Whether these laws are a matter of clarification or contradiction is the matter of some debate. \u0000RÉSUMÉL'extraction de ressources naturelles situées au-delà de la Terre pour créer des produits peut être décrite comme une utilisation des ressources spatiales (URS). L’URS est actuellement examinée à la fois dans les secteurs public et privé. Les astéroïdes proches de la Terre (NEA) sont des cibles URS particulièrement prometteuses en raison de leur proximité relative et de leur enrichissement en deux ressources clés : l’eau et les éléments du groupe du platine (EGP). L'eau peut être utilisée pour créer des agents de propulsion pour vaisseaux spatiaux, ce qui en fait la seule ressource pour laquelle la demande est importante compte tenu de l’émergence du marché spatial actuel. Les EGP sont suffisamment précieux pour que leur importation sur le marché terrestre soit potentiellement économique, ce qui en fait l’autre ressource potentielle étant donné l’état embryonnaire actuel de l’URS. Bien qu'il soit possible de récupérer des matériaux sur un NEA, le faire à une échelle économique nécessitera des développements importants dans des domaines tels que la robotique autonome et la technologie de propulsion. Un paramétrage tenant compte de la taille des astéroïdes, de la concentration des ressources et de l'accessibilité conduit à seulement sept et trois cibles NEA parmi la population c","PeriodicalId":55106,"journal":{"name":"Geoscience Canada","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-07-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42550491","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Great Mining Camps of Canada 6. Geology and History of the Wabana Iron Mines, Bell Island, Newfoundland","authors":"Jeffrey Pollock","doi":"10.12789/GEOCANJ.2019.46.148","DOIUrl":"https://doi.org/10.12789/GEOCANJ.2019.46.148","url":null,"abstract":"The Wabana iron mines were in operation from 1895 to 1966, during which time they produced over 80 million tonnes of iron ore. They are hosted by Early Ordovician rocks that contain Clinton-type stratiform ironstones. Mineralization is characterized by oölitic, dark red to purple-red to reddish brown beds of hematite-rich fossiliferous sandstone, siltstone, and shale. Three ironstone beds are of economic importance: the Lower (Dominion Formation), Middle (Scotia Formation) and Upper (Gull Island Formation) with the Lower bed extending over 3.8 km beneath Conception Bay. The iron content in all beds ranges from 45 to 61% with a silica concentration of 6 to 20%.   Reports of iron on Bell Island go back to at least 1578, when a Bristol merchant reported retrieving ore samples for shipment to England. The deposits, however, remained undeveloped for over three centuries until their rediscovery by local fishermen in the late 1880s. In 1895, the Nova Scotia Steel & Coal Company acquired the mining lease for the claims and first ore was produced at surface from No. 1 mine in the Lower bed along the island’s northwest coast. By the turn of the twentieth century the Dominion Iron and Steel Company Limited acquired a share of the Bell Island claims, and with surface reserves exhausted, the decision was made by both companies to proceed underground and develop submarine mines. Over the next five decades mining operations were operated by several owners at a steady and at times an expanding rate, with periodic setbacks through two world wars and the Great Depression. The worldwide increase in demand for iron after World War II meant the mines were in full production and exporting over 1.5 million tonnes of ore per annum. In 1950, the unprofitable No. 2 mine was closed, and a series of major expansion projects were launched with the goal to double annual production to 3 million tonnes.   By the 1960s, the Wabana mines faced increased competition from foreign producers, who flooded the world iron market with high-quality ore from low-cost open-pit deposits. The last mine at Wabana ceased operation in 1966 because the high-phosphorus content of the ore was incompatible with the newest steel-making technology and the market for Wabana ore all but disappeared. Over 35 million tonnes of ore was exported to Canada (Nova Scotia) while the remainder was shipped to the United Kingdom and Germany. At the time of closure, the Wabana mines were the oldest, continually producing mine in the country. Annual production peaked in 1960 when over 2.8 million tonnes of concentrated ore were shipped. Enormous potential reserves of several billion tonnes, grading 50% iron, remain in place beneath Conception Bay but the high cost of submarine mining and absence of a market for non-Bessemer ore present obstacles to any future re-development. \u0000RÉSUMÉLes mines de fer de Wabana ont été en activité de 1895 à 1966, période durant laquelle elles ont produit plus de 80 millions de tonnes d","PeriodicalId":55106,"journal":{"name":"Geoscience Canada","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-07-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43370038","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Geoscience Canada — Forty-Five Years Young","authors":"A. Kerr","doi":"10.12789/GEOCANJ.2019.46.142","DOIUrl":"https://doi.org/10.12789/GEOCANJ.2019.46.142","url":null,"abstract":"","PeriodicalId":55106,"journal":{"name":"Geoscience Canada","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-03-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42737395","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Age, Geochemistry and Origin of the Ardara Appinite Plutons, Northwest Donegal, Ireland","authors":"J. Murphy, R. Nance, Logan B. Gabler, A. Martell, D. Archibald","doi":"10.12789/GEOCANJ.2019.46.144","DOIUrl":"https://doi.org/10.12789/GEOCANJ.2019.46.144","url":null,"abstract":"In northwest Donegal, Ireland, a large number of coeval appinitic (hornblende-plagioclase-rich) plutons and lamprophyre dykes occur around the Ardara pluton, a granitic satellite body and one of the oldest phases of the ca. 428–400 Ma composite Donegal Batholith. The appinite units form a bimodal (mafic–felsic) suite in which hornblende is the dominant mafic mineral and typically occurs as large prismatic phenocrysts within a finer grained matrix. Lamprophyre dykes are mafic in composition with a geochemistry that is very similar to that of the mafic appinite bodies. Both mafic rocks are subalkalic, with calc-alkalic and tholeiitic tendencies, and show trace element abundances indicating that the mantle source was contaminated by subduction zone fluids. 40Ar/39Ar analysis of hornblende separated from two samples of appinite yield mid-Silurian (434.2 ± 2.1 Ma and 433.7 ± 5.5 Ma) cooling ages that are interpreted to closely date the time of intrusion. Hence, according to the available age data, the appinite bodies slightly predate, or were coeval with, the earliest phases of the Donegal Batholith. Sm–Nd isotopic analyses yield a range of initial εNd values (+3.1 to –4.8 at t = 435 Ma) that, together with trace element data, indicate that the appinitic magmas were likely derived from melting of metasomatized sub-continental lithospheric mantle and/or underplated mafic crust, with only limited crustal contamination during magma ascent. The appinitic intrusions are interpreted to have been emplaced along deep-seated crustal fractures that allowed for mafic and felsic magma to mingle. The magmas are thought to be the products of collisional asthenospheric upwelling associated with the closure of Iapetus and the ensuing Caledonian orogeny, either as a result of an orogen-wide delamination event or as a consequence of more localized slab break-off.RÉSUMÉDans le nord-ouest du Donegal, en Irlande, un grand nombre de plutons appinitiques (riches en hornblendes ou en plagioclases) et de dykes de lamprophyres contemporains se retrouvent autour du pluton d’Ardara, un corps satellite granitique et l’une des phases les plus anciennes du batholite composite de Donegal, âgé d’environ 428–400 Ma. Les unités de l’appinite forment une suite bimodale (mafique–felsique) dans laquelle la hornblende est le minéral mafique dominant et se présente généralement sous forme de grands phénocristaux prismatiques au sein d’une matrice à grains plus fins. Les dykes de lamprophyres ont une composition mafique dont la géochimie est très similaire à celle des corps d’appinite mafique. Les deux roches mafiques sont subalcaliques, avec des tendances calcoalcalines et tholéiitiques, et elles montrent des teneurs en éléments traces indiquant que la source du manteau a été contaminée par des fluides de zone de subduction. L'analyse 40Ar/39Ar des hornblendes provenant de deux échantillons d'appinite donne des âges de refroidissement du Silurien moyen (434,2 ± 2,1 Ma et 433,7 ± 5,5 Ma) qui","PeriodicalId":55106,"journal":{"name":"Geoscience Canada","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-03-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"44707974","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Thank You to 2017–2018 Guest Editors and Reviewers","authors":"","doi":"10.12789/geocanj.2019.46.146","DOIUrl":"https://doi.org/10.12789/geocanj.2019.46.146","url":null,"abstract":"","PeriodicalId":55106,"journal":{"name":"Geoscience Canada","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-03-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42227462","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}