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Littérature scientifique sur le sujet « Eastern North American margin »

Auteur : Grafiati

Publié le 4 juin 2021

Mis à jour le 3 février 2022

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Articles de revues sur le sujet "Eastern North American margin"

Savage, B., B. M. Covellone et Y. Shen. « Wave speed structure of the eastern North American margin ». Earth and Planetary Science Letters 459 (février 2017) : 394–405. http://dx.doi.org/10.1016/j.epsl.2016.11.028.

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Servali, Andrea, Maureen D. Long, Jeffrey Park, Margaret H. Benoit et John C. Aragon. « Love-to-Rayleigh scattering across the eastern North American passive margin ». Tectonophysics 776 (février 2020) : 228321. http://dx.doi.org/10.1016/j.tecto.2020.228321.

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Lynner, Colton, Harm J. A. Van Avendonk, Anne Bécel, Gail L. Christeson, Brandon Dugan, James B. Gaherty, Steven Harder et al. « The Eastern North American Margin Community Seismic Experiment : An Amphibious Active‐ and Passive‐Source Dataset ». Seismological Research Letters 91, n^o 1 (30 octobre 2019) : 533–40. http://dx.doi.org/10.1785/0220190142.

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Abstract The eastern North American margin community seismic experiment (ENAM‐CSE) was conceived to target the ENAM Geodynamic Processes at Rifting and Subducting Margins (GeoPRISMS) primary site with a suite of both active‐ and passive‐source seismic data that would shed light on the processes associated with rift initiation and evolution. To fully understand the ENAM, it was necessary to acquire a seismic dataset that was both amphibious, spanning the passive margin from the continental interior onto the oceanic portion of the North American plate, and multiresolution, enabling imaging of the sediments, crust, and mantle lithosphere. The ENAM‐CSE datasets were collected on‐ and offshore of North Carolina and Virginia over a series of cruises and land‐based deployments between April 2014 and June 2015. The passive‐source component of the ENAM‐CSE included 30 broadband ocean‐bottom seismometers (OBSs) and 3 onshore broadband instruments. The broadband stations were deployed contemporaneously with those of the easternmost EarthScope Transportable Array creating a trans‐margin amphibious seismic dataset. The active‐source portion of the ENAM‐CSE included several components: (1) two onshore wide‐angle seismic profiles where explosive shots were recorded on closely spaced geophones; (2) four major offshore wide‐angle seismic profiles acquired with an airgun source and short‐period OBSs (SPOBSs), two of which were extended onland by deployments of short‐period seismometers; (3) marine multichannel seismic (MCS) data acquired along the four lines of SPOBSs and a series of other profiles along and across the margin. During the cruises, magnetic, gravity, and bathymetric data were also collected along all MCS profiles. All of the ENAM‐CSE products were made publicly available shortly after acquisition, ensuring unfettered community access to this unique dataset.

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Mazza, Sarah E., Esteban Gazel, Elizabeth A. Johnson, Michael Bizimis, Ryan McAleer et C. Berk Biryol. « Post-rift magmatic evolution of the eastern North American “passive-aggressive” margin ». Geochemistry, Geophysics, Geosystems 18, n^o 1 (janvier 2017) : 3–22. http://dx.doi.org/10.1002/2016gc006646.

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Lynner, Colton, et Robert W. Porritt. « Crustal structure across the eastern North American margin from ambient noise tomography ». Geophysical Research Letters 44, n^o 13 (3 juillet 2017) : 6651–57. http://dx.doi.org/10.1002/2017gl073500.

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Lynner, Colton, et Miles Bodmer. « Mantle flow along the eastern North American margin inferred from shear wave splitting ». Geology 45, n^o 10 (4 août 2017) : 867–70. http://dx.doi.org/10.1130/g38980.1.

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Attias, Eric, Rob L. Evans, Samer Naif, Jimmy Elsenbeck et Kerry Key. « Conductivity structure of the lithosphere-asthenosphere boundary beneath the eastern North American margin ». Geochemistry, Geophysics, Geosystems 18, n^o 2 (février 2017) : 676–96. http://dx.doi.org/10.1002/2016gc006667.

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Long, Maureen D., Margaret H. Benoit, Rob L. Evans, John C. Aragon et James Elsenbeck. « The MAGIC Experiment : A Combined Seismic and Magnetotelluric Deployment to Investigate the Structure, Dynamics, and Evolution of the Central Appalachians ». Seismological Research Letters 91, n^o 5 (1 juillet 2020) : 2960–75. http://dx.doi.org/10.1785/0220200150.

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Abstract The eastern margin of North America has undergone multiple episodes of orogenesis and rifting, yielding the surface geology and topography visible today. It is poorly known how the crust and mantle lithosphere have responded to these tectonic forces, and how geologic units preserved at the surface related to deeper structures. The eastern North American margin has undergone significant postrift evolution since the breakup of Pangea, as evidenced by the presence of young (Eocene) volcanic rocks in western Virginia and eastern West Virginia and by the apparently recent rejuvenation of Appalachian topography. The drivers of this postrift evolution, and the precise mechanisms through which relatively recent processes have modified the structure of the margin, remain poorly understood. The Mid-Atlantic Geophysical Integrative Collaboration (MAGIC) experiment, part of the EarthScope USArray Flexible Array, consisted of collocated, dense, linear arrays of broadband seismic and magnetotelluric (MT) stations (25–28 instruments of each type) across the central Appalachian Mountains, through the U.S. states of Virginia, West Virginia, and Ohio. The goals of the MAGIC deployment were to characterize the seismic and electrical conductivity structure of the crust and upper mantle beneath the central Appalachians using natural-source seismic and MT imaging methods. The MAGIC stations operated between 2013 and 2016, and the data are publicly available via the Incorporated Research Institutions for Seismology Data Management Center.

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SHEARD, John W., Alexander K. EZHKIN, Irina A. GALANINA, Dmitry HIMELBRANT, Ekaterina KUZNETSOVA, Akira SHIMIZU, Irina STEPANCHIKOVA et al. « The lichen genusRinodina(Physciaceae,Caliciales) in north-eastern Asia ». Lichenologist 49, n^o 6 (novembre 2017) : 617–72. http://dx.doi.org/10.1017/s0024282917000536.

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AbstractRinodinais a widespread, polyphyletic genus of crustosePhysciaceaewithc. 300 species worldwide. A major missing link in understanding its global biogeography has been eastern Asia where the genus has never been systematically revised. Here we review specimen and literature records forRinodinafor north-eastern Asia (Russian Far East, Japan and the Korean Peninsula) and recognize 43 species. We describe two species,R. hypobadiaandR. orientalis, as new to science.Rinodina hypobadiais distinguished by its pigmented hypothecium,Dirinaria-type ascospores and pannarin in both thallus and epihymenium.Rinodina orientalisis characterized by its erumpent apothecia that remain broadly attached, with discs sometimes becoming convex and excluding the thalline margins, ascospores belonging to thePhyscia-type and secondary metabolites absent. Nine other species are reported from the region for the first time. These includeR. dolichospora,R. freyi,R. metaboliza,R. sicula,R. subminutaandR. willeyi. Of particular biogeographical interest are three additional new records that have western North American–eastern Asian distributions: the corticolous speciesR. endospora,R. macrosporaandR. megistospora. Six species have the better known eastern North American–eastern Asian distributions:R. ascociscana(syn.R. akagiensis,R. melancholica),R. buckii,R. chrysidiata,R. subminuta,R. tenuis(syn.R. adirondackii) andR. willeyi, and two have eastern North American–eastern Asian–European distributions:R. excrescensandR. moziana(syn.R. destituta,R. vezdae). Our study begins to close one of the largest gaps in our knowledge of circumboreal species distributions inRinodinaand, together with previous studies in North America and Europe, provides new insights into circumboreal crustose lichen biogeography.Rinodina cinereovirens(syn.R. turfaceavar. cinereovirens) is also reported as new to North America.

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Falkowski, P. G., P. E. Biscaye et C. Sancetta. « The lateral flux of biogenic particles from the eastern North American continental margin to the North Atlantic Ocean ». Deep Sea Research Part II : Topical Studies in Oceanography 41, n^o 2-3 (janvier 1994) : 583–601. http://dx.doi.org/10.1016/0967-0645(94)90036-1.

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Thèses sur le sujet "Eastern North American margin"

Lynner, Colton, et Robert W. Porritt. « Crustal structure across the eastern North American margin from ambient noise tomography ». AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/625356.

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Passive tectonic margins, like the eastern North American margin (ENAM), represent the meeting of oceanic and continental material where no active deformation is occurring. The recent ENAM Community Seismic Experiment provides an opportunity to examine the crustal structure across the ENAM owing to the simultaneous deployment of offshore and onshore seismic instrumentation. Using Rayleigh wave phase and group velocities derived from ambient noise data, we invert for shear velocity across the ENAM. We observe a region of transitional crustal thicknesses that connects the oceanic and continental crusts. Associated with the transitional crust is a localized positive gravitational anomaly. Farther east, the East Coast magnetic anomaly (ECMA) is located at the intersection of the transitional and oceanic crusts. We propose that underplating of dense magmatic material along the bottom of the transitional crust is responsible for the gravitational anomaly and that the ECMA demarks the location of initial oceanic crustal formation.

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Cornell, Sean Richard. « The Last Stand of the Great American Carbonate Bank : Tectonic Activation of the Upper Ordovician Passive Margin in Eastern North America ». Cincinnati, Ohio : University of Cincinnati, 2008. http://rave.ohiolink.edu/etdc/view.cgi?acc_num=ucin1226880226.

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Thesis (Ph.D.)--University of Cincinnati, 2008.
Advisor: Dr. Carlton Brett PhD (Advisor), Dr. Warren Huff PhD (Committee Member), Dr. J.B. Maynard PhD (Committee Member), Dr. Thomas Algeo PhD (Committee Member), Dr. Brian Witzke PhD (Committee Member), Dr. Kees Dejong PhD (Committee Member). Title from electronic thesis title page (viewed Feb. 3, 2009). Keywords: sequence stratigraphy; ordovician; taconic orogeny; blountian tectophase; chemostratigraphy; strontium isotopes; time restricted facies; mohawkian; trenton group; black river group; chazy group. Includes abstract. Includes bibliographical references.

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Leatham, W. Britt. « Conodont-based chronostratigraphy and conodont distribution across the Upper Ordovician western North American carbonate platform in the eastern Great Basin and a model for Ordovician-Silurian Genesis of the platform margin based ... / ». The Ohio State University, 1987. http://rave.ohiolink.edu/etdc/view?acc_num=osu1487332636474718.

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Speer, William D. « Systematics of Eastern North American Bracken Fern ». Thesis, Virginia Tech, 1997. http://hdl.handle.net/10919/36715.

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The cosmopolitan Pteridium aquilinum (L.) Kuhn is widespread throughout eastern North American, where it is represented primarily by Tryon's (1941) var. latiusculum (Desv.) Underw. and var. pseudocaudatum (Clute) Heller. The taxonomy of Pteridium is controversial. Fourteen isozyme loci and 12 morphological characters were used to assess the taxonomic relationship of these two varieties. Isozyme data indicated a high mean genetic identity (I = 0.976) between eleven bracken populations. Strong patterns of geographic variation for isozyme allele frequencies were also observed. The isozyme results did not separate the two taxa. Numerical analysis of the morphology distinguished the two taxa when the qualitative characters were used alone or in conjunction with some of the quantitative traits. All qualitative characters differed significantly between the two taxa. No perceptible geographic pattern of variation was observed. Morphological distinctiveness was maintained even in those localities where both taxa were present, with few or no intermediates being found. Isozyme evidence suggestive of gene flow between the two varieties was found at Greensboro, NC, where the two morphotypes were easily recognizable. The isozyme evidence strongly indicates conspecificity, while the morphological evidence supports their status at the varietal level.
Master of Science

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Rodger, Matthew. « A marine geophysical study of the Amazon continental margin, North-Eastern Brazil ». Thesis, University of Oxford, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.504519.

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Francavilla, Stephen A. « Millennial-scale variability in denitrification and phosphorus burial in the Eastern Tropical North Pacific ». Thesis, University of Edinburgh, 2009. http://hdl.handle.net/1842/3860.

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The remarkable synchrony between changes in temperature recorded in Greenland ice cores and variations in N isotope records from sedimentary cores recovered from the Arabian Sea and the Eastern Tropical North Pacific (ETNP) has provided evidence for teleconnections between changes in marine denitrification in the tropics and climate variations in the northern high latitudes. Changes in tropical denitrification have been attributed to changes in productivity, changes in the source of intermediate waters and the flux of dissolved oxygen to suboxic zones. Variations in marine denitrification and anammox occurring at intermediate depths in proximity to productive continental margins have had profound effects on the N:P ratio of upwelled waters between stadials and interstadials, and may have indirectly affected carbon sequestration in the ocean by changing the balance of nutrients available to primary productivity. Competitive equilibrium, the changing stoichiometric balance of elements available as nutrients and the shorter residence time of N compared to P are factors that are believed to favour diazotrophs (N2-fixing organisms) during interstadials and shift the competitive advantage to non-N2-fixing ecosystems during stadials. This study presents a very high-resolution analysis of sedimentary nitrogen isotope records, phosphorus concentrations and bulk detrital element concentrations from two cores collected along the Pacific Mexican Margin. The results show that the oxygen minimum zone (OMZ) bathing intermediate waters in ETNP is modulated by the interaction of a Northern Hemisphere climate component with the “leakage” of heavy nitrate believed to derive from the Eastern South Pacific (ESP). This southerly component has a more “Antarctic” timing and is similar to records from the Peru-Chile margin. The sedimentary core recovered from the Mazatlan margin shows a “Greenland” timing of millennial-scale events, with reduced upwelling and reduced primary productivity, a less intense OMZ leading to reduced denitrification and a more southerly position of the mid-tropospheric subtropical ridge during stadials. This would have increased the onshore flow of moist air, ultimately leading to increased precipitation along the western Mexican Margin. Interstadials show a reversal of these conditions. In contrast to the Mazatlan core, the N isotope record from the core recovered from the Gulf of Tehuantepec records an element of “Antarctic” timing superimposed on local, millennial-scale variations in denitrification that are more similar in timing to Greenland temperature changes. In addition, the interpretation of observed variations in detrital elements from the Gulf of Tehuantepec highlights latitudinal displacements of the ITCZ that are consistent with those observed in the Cariaco Basin in Venezuela. Bulk P concentrations from both cores suggest that although phosphorite formation in the ETNP during interstadials is not as widespread as previously thought, the very high accumulation rates in the Gulf of Tehuantepec and Mazatlan Margin lead to total Holocene phosphorus burial rates that are up to 4-5 times higher than had been estimated in previous studies. These observations lead to the argument that the ETNP may play a more important role in regulating global P budgets than was previously thought and call for an improved appreciation of the benthic microbial communities that modulate biomes at tropical latitudes.

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Nameroff, Tamara J. « Suboxic trace metal geochemistry and paleo-record in continental margin sediments of the eastern tropical North Pacific / ». Thesis, Connect to this title online ; UW restricted, 1996. http://hdl.handle.net/1773/8514.

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Allin, Joshua Reg. « The timing and frequency of large-volume submarine landslides and turbidity currents along the north-eastern Atlantic Margin ». Thesis, University of Southampton, 2016. https://eprints.soton.ac.uk/407493/.

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Submarine landslides and turbidity currents are one of the most voluminous sediment transport mechanisms operating on our planet. Due to their potential size (>100 km3) and speed (>20 m/s) they pose considerable risk to coastal settlements and strategic marine infrastructure. This thesis aims to investigate the processes that precondition and trigger submarine landslides and turbidity currents within submarine canyons and on open continental slopes. Sediment cores, age models, and statistical analyses are used initially to test the effects of eustatic sea level on the recurrence rates of turbidity currents that fill and flush the Nazaré Canyon. Recurrence rates of turbidity currents that fill the canyon are strongly influenced by eustatic sea level, while more infrequent flows that flush the canyon are only associated with shifts in eustatic sea level periodicity and amplitude. The form of the frequency distribution of canyon filling and flushing turbidity currents also differ markedly, suggesting they have different triggers. This thesis also aims to understand the geohazard implications of large submarine landslides. The Trænadjupet Slide is a large ( > 400 km3) submarine landslide that occurred approximately 4,000 years ago on the Norwegian Margin. Unlike some other large submarine landslides, the Trænadjupet Slide did not trigger a widespread tsunami based on available coastal studies. The age of the Trænadjupet Slide is refined here to between ~2,600 and ~3,400 cal BP. The absence of a widespread tsunami associated with the Trænadjupet Slide may be explained by its emplacement dynamics (e.g. speed, acceleration, or time gaps between stages of failure). These findings have importance for landslide geohazards in the North Atlantic, as they suggest that other similarly-sized slides on the Norwegian Margin or elsewhere may not have produced very damaging tsunamis.

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Haines, Helen Rozeann. « Intra-site obsidian distribution and consumption patterns in Northern Belize and the North-Eastern Peten ». Thesis, University College London (University of London), 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.325664.

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Lowe, Charles H., R. Roy Johnson et Peter S. Bennett. « Riparianlands are Wetlands : The Problem of Applying Eastern American Concepts and Criteria to Environments in the North American Southwest ». Arizona-Nevada Academy of Science, 1986. http://hdl.handle.net/10150/296391.

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From the Proceedings of the 1986 Meetings of the Arizona Section - American Water Resources Association, Hydrology Section - Arizona-Nevada Academy of Science and the Arizona Hydrological Society - April 19, 1986, Glendale Community College, Glendale, Arizona

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Livres sur le sujet "Eastern North American margin"

Cenozoic seas : The view from eastern North America. Boca Raton, Fla : CRC Press, 2004.

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Drass, Richard. Culture change on the eastern margins of the southern plains. [Norman, Okla.] : Oklahoma Archeological Survey, University of Oklahoma, 1997.

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Krupat, Arnold. The voice in the margin : Native American literature and the canon. Berkeley : University of California Press, 1989.

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Canada, Geological Survey of. Ancient Western North American Margin : An Alpine Rift Model For the East-Central Canadian Cordillera. S.l : s.n, 1987.

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A, Niering William, Olmstead Nancy C et National Audubon Society, dir. National Audubon Society field guide to North American wildflowers : Eastern region. New York : Alfred A. Knopf, 2001.

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Diamond, Beverley. Native American music in eastern North America : Experiencing music, expressing culture. New York : Oxford University Press, 2008.

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Atmospheric sulfur and nitrogen oxides : Eastern North American source-receptor relationships. San Diego : Academic Press, 1994.

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Struik, L. C. The ancient western North American margin : An alpine rift model for the east-central Canadian Cordillera. Ottawa, Canada : Geological Survey of Canada, 1987.

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Folkens, Pieter A. Marine mammals of the eastern North Pacific, including southern Alaska, the west coast of North America, Hawaiian Islands, and Gulf of California : A concise and comprehensive waterproof guide. [United States?] : A Higher Porpoise Design Group, 2000.

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Folkens, Pieter A. Marine mammals of the eastern North Pacific, including southern Alaska, the west coast of North America, Hawaiian Islands, and the Sea of Cortez : A concise and comprehensive waterproof guide. [Corvallis, Or.] : Marine Mammal Program, Oregon State University and Oregon Sea Grant, 2000.

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Chapitres de livres sur le sujet "Eastern North American margin"

Adams, John, et Peter W. Basham. « Seismicity and Seismotectonics of Canada’s Eastern Margin and Craton ». Dans Earthquakes at North-Atlantic Passive Margins : Neotectonics and Postglacial Rebound, 355–70. Dordrecht : Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2311-9_21.

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Mehra-Palta, Asha, et David G. Thompson. « Tissue Culture of Eastern North American Conifers ». Dans Cell and Tissue Culture in Forestry, 61–79. Dordrecht : Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-017-0992-7_5.

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Meltzer, David J. « Was Stone Exchanged Among Eastern North American Paleoindians ? » Dans Eastern Paleoindian Lithic Resource Use, 11–39. New York : Routledge, 2021. http://dx.doi.org/10.4324/9780429049743-2.

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Basham, P. W. « Problems with Seismic Hazard Assessment on the Eastern Canadian Continental Margin ». Dans Earthquakes at North-Atlantic Passive Margins : Neotectonics and Postglacial Rebound, 679–86. Dordrecht : Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2311-9_38.

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Stevens, Anne E. « Damage associated with three early Eastern North American earthquakes ». Dans Earthquake Engineering, sous la direction de Shamim A. Sheikh et S. M. Uzumeri, 807–14. Toronto : University of Toronto Press, 1991. http://dx.doi.org/10.3138/9781487583217-102.

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Belardi, Juan Bautista, Flavia Carballo Marina et Gustavo Barrientos. « Hunting Landscapes in the North Margin of Lake Viedma (Southern Patagonia, Argentina) : Preys, Strategies and Technology ». Dans The Latin American Studies Book Series, 343–60. Cham : Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-61187-3_13.

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Kneeshaw, Daniel, Philip J. Burton, Louis De Grandpré, Sylvie Gauthier et Yan Boulanger. « Is Management or Conservation of Old Growth Possible in North American Boreal Forests ? » Dans Ecology and Recovery of Eastern Old-Growth Forests, 139–57. Washington, DC : Island Press/Center for Resource Economics, 2018. http://dx.doi.org/10.5822/978-1-61091-891-6_8.

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Symons, D. T. A., et M. T. Lewchuk. « Paleomagnetism of the Mississippian HP Pipe and the Western Margin of the North American Craton ». Dans Deep Structure and Past Kinematics of Accreted Terranes, 113–25. Washington, D. C. : American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm050p0113.

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Occhibove, Flavia, Claudia Ferro, Marco Campera, Gian Battista Liponi, Silvana M. Borgognini-Tarli, Joerg U. Ganzhorn et Giuseppe Donati. « Living in Islands of Forests : Nutritional Ecology of the Howler Monkey (Alouatta palliata) at La Suerte Biological Field Station, North-Eastern Costa Rica ». Dans Central American Biodiversity, 525–38. New York, NY : Springer New York, 2015. http://dx.doi.org/10.1007/978-1-4939-2208-6_22.

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Ettensohn, Frank R. « Geologic Origins of the North American Shale-Gas Revolution : Can it Happen Elsewhere ? » Dans Paleobiodiversity and Tectono-Sedimentary Records in the Mediterranean Tethys and Related Eastern Areas, 279–81. Cham : Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01452-0_67.

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Actes de conférences sur le sujet "Eastern North American margin"

Ebel, John E., et Martin C. Chapman. « EASTERN NORTH AMERICA PASSIVE MARGIN EARTHQUAKES AND MESOZOIC RIFT STRUCTURES ». Dans Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-343949.

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Withjack, Martha O., et LeeAnn Srogi. « LATERAL TRANSPORT OF CAMP-RELATED MAGMAS BENEATH THE EASTERN NORTH AMERICAN RIFT SYSTEM AND MARGIN ». Dans GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355723.

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Li, Cong, et Haiying Gao. « MODIFICATION OF CRUST AND MANTLE LITHOSPHERE BENEATH THE SOUTHERN PART OF THE EASTERN NORTH AMERICAN PASSIVE MARGIN ». Dans GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-351422.

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Foster-Baril, Zachary, Daniel F. Stockli et Christopher M. Bailey. « PROVENANCE OF THE TRIASSIC TO JURASSIC NEWARK SUPERGROUP DURING PROGRESSIVE RIFTING ALONG THE EASTERN NORTH AMERICAN MARGIN, USA ». Dans Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-345221.

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Cooper Boemmels, Jennifer, Jean Crespi, Thomas H. Fleming et Laura E. Webb. « EARLY CRETACEOUS POSTRIFT EVOLUTION OF THE EASTERN NORTH AMERICAN MARGIN : INSIGHTS FROM THE NEW ENGLAND-QUEBEC IGNEOUS PROVINCE ». Dans GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-336121.

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Cooper Boemmels, Jennifer, Jean Crespi et Thomas H. Fleming. « EARLY CRETACEOUS MAGMATISM IN WESTERN VERMONT AND EASTERN NEW YORK : TIMING, GEOCHEMISTRY, AND ROLE IN THE POSTRIFT EVOLUTION OF THE EASTERN NORTH AMERICAN MARGIN ». Dans 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328580.

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Kinney, Sean T., Scott A. Maclennan, Jacob Setera, Blair Schoene, Jill VanTongeren, Justin V. Strauss, Dwight Bradley, Austin Hart, Caleb Forrest Town et Paul E. Olsen. « LONG-LIVED AND LOCALIZED POST-OROGENIC MAGMATISM ON THE EASTERN NORTH AMERICAN MARGIN : INSIGHTS FROM ZIRCON U-PB GEOCHRONOLOGY ». Dans Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-345449.

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Luckie, Thomas W., Lindsay Lowe Worthington et M. Beatrice Magnani. « INITIAL RESULTS FROM THE EASTERN NORTH AMERICA MARGIN COMMUNITY SEISMIC EXPERIMENT ONSHORE ACTIVE SOURCE SEISMIC DATA ». Dans GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-284768.

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Menke, William, Dallas Abbott et Vadim Levin. « THE INFLUENCE OF MANTLE UPWELLING AT THE PASSIVE CONTINENTAL MARGIN OF EASTERN NORTH AMERICA ON THE CRUST ». Dans 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-327907.

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Cooper Boemmels, Jennifer, Jean Crespi, Will Amidon, Thomas H. Fleming et Laura E. Webb. « EARLY CRETACEOUS POSTRIFT MAGMATISM AND NORMAL FAULTING IN THE NORTHERN APPALACHIANS : IMPLICATIONS FOR THE EVOLUTION OF THE EASTERN NORTH AMERICAN MARGIN ». Dans GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-356541.

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Rapports d'organisations sur le sujet "Eastern North American margin"

Kosro, P. M., et Robert L. Smith. Moored Current Measurements Over the Continental Slope of the Ocean's Eastern Boundary & ; An Investigation of the Poleward Undercurrent Over the Continental Margin of North America. Fort Belvoir, VA : Defense Technical Information Center, septembre 1997. http://dx.doi.org/10.21236/ada627890.

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Struik, L. C. The Ancient western North American Margin : An Alpine Rift Model For the East - Central Canadian Cordillera. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122388.

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Jansa, L. F., et G. Pe-Piper. Geology and Geochemistry of Middle Jurassic and Early Cretaceous Igneous Rocks On the eastern North American Continental Shelf. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130140.

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Gillis, R. J., D. L. LePain, R. R. Reifenstuhl et K. P. Helmold. Regional Paleocene-Eocene exhumation of the North American forearc basin margin, south-central Alaska, recorded by apatite fission-track thermochronology (poster) : Geological Society of America Abstracts with Programs, Vol. 41, No. 7. Alaska Division of Geological & Geophysical Surveys, 2009. http://dx.doi.org/10.14509/21163.

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