Bibliografías temáticas / Greenland evolution

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Literatura académica sobre el tema "Greenland evolution"

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Publicado: 4 de junio de 2021

Última modificación: 5 de febrero de 2022

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Artículos de revistas sobre el tema "Greenland evolution"

Benoit, France y Gunnar Martens. "Municipal government in Greenland". Polar Record 28, n.º 165 (abril de 1992): 93–104. http://dx.doi.org/10.1017/s0032247400013383.

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AbstractThis article describes how Greenlandic municipalities operate. A summary of the evolution of municipal government in Greenland is followed by an overview of their demography, politics, and administration. A list of jurisdictions is provided through a study of municipal expenditures, with reference to the municipality of Narsaq (Narsap kommunia). The article concludes with an examination of the perspectives of municipal government in Greenland.

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Lahtinen, Raimo, Adam A. Garde y Victor A. Melezhik. "Paleoproterozoic evolution of Fennoscandia and Greenland". Episodes 31, n.º 1 (1 de marzo de 2008): 20–28. http://dx.doi.org/10.18814/epiiugs/2008/v31i1/004.

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Perner, K., M. Moros, A. Jennings, JM Lloyd y KL Knudsen. "Holocene palaeoceanographic evolution off West Greenland". Holocene 23, n.º 3 (18 de octubre de 2012): 374–87. http://dx.doi.org/10.1177/0959683612460785.

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Jess, Scott, Alexander L. Peace y Christian Schiffer. "Sediment supply on the West Greenland passive margin: redirection of a large pre-glacial drainage system". Journal of the Geological Society 177, n.º 6 (8 de julio de 2020): 1149–60. http://dx.doi.org/10.1144/jgs2020-028.

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The Mesozoic–Cenozoic separation of Greenland and North America produced the small oceanic basins of the Labrador Sea and Baffin Bay, connected via a complex transform system through the Davis Strait. During rifting and partial breakup sedimentary basins formed that record the changing regional sediment supply. The onshore and offshore stratigraphy of Central West Greenland outlines the presence of a major fluvial system that existed during the Cretaceous and was later redirected in the Early Cenozoic by the formation of the West Greenland Igneous Province. Hydrological analysis of Greenland's isostatically balanced basement topography outlines two major drainage systems that likely flowed across Greenland prior to the onset of glaciation and emptied into the Sisimiut Basin within the Davis Strait, offshore West Greenland. The course of the northern drainage system suggests that it initially flowed NW into the Cretaceous/Palaeocene Nuussuaq Basin, before being redirected SW around the West Greenland Igneous Province in the Mid-Palaeocene. Moreover, characteristics of these two drainage systems suggest they acted as a single larger fluvial system, prior to the onset of glaciation, that was likely the primary source of sediment across Central West Greenland throughout the Cretaceous and Palaeogene. This scenario provides a greater understanding of the West Greenland margin's late Cenozoic evolution, which differs from previous interpretations that hypothesize a period of considerable post-rift tectonism and uplift. This work highlights the importance of large pre-glacial drainage systems across North Atlantic passive margins and their relevance when studying post-rift stratigraphy in rifted margin settings.Supplementary material: Isostatic modelling, hydrological analysis and chi mapping is available at: https://doi.org/10.6084/m9.figshare.c.5050146

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Surlyk, F. "Tectonostratigraphy of North Greenland". Bulletin Grønlands Geologiske Undersøgelse 160 (1 de enero de 1991): 25–47. http://dx.doi.org/10.34194/bullggu.v160.6712.

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A coherent tectonic and stratigraphic picture of the geological evolution of North Greenland has emerged after a decade of systematic mapping and topical studies by the Geological Survey of Greenland (GGU) in cooperation with groups from the University of Copenhagen and various non-Danish institutions. These studies represent the culmination of a long exploration history, with field work often carried out under harsh conditions.

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Gregersen, Ulrik, Paul C. Knutz, Henrik Nøhr-Hansen, Emma Sheldon y John R. Hopper. "Tectonostratigraphy and evolution of the West Greenland continental margin". Bulletin of the Geological Society of Denmark 67 (27 de julio de 2020): 1–21. http://dx.doi.org/10.37570/bgsd-2019-67-01.

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Large structural highs and sedimentary basins are identified from mapping of the West Greenland continental margin from the Labrador Sea to the Baffin Bay. We present a new tectonic elements map and a map of thickness from the seabed to the basement of the entire West Greenland margin. In addition, a new stratigraphic scheme of the main lithologies and tectonostratigraphy based on ties to all offshore exploration wells is presented together with seven interpreted seismic sections. The work is based on interpretation of more than 135 000 km of 2D seismic reflection data supported by other geophysical data, including gravity- and magnetic data and selected 3D seismic data, and is constrained by correlation to wells and seabed samples. Eight seismic mega-units (A–H) from the seabed to the basement, related to distinct tectonostratigraphic phases, were mapped. The oldest units include pre-rift basins that contain Proterozoic and Palaeozoic successions. Cretaceous syn-rift phases are characterised by development of large extensional fault blocks and basins with wedge-shaped units. The basin strata include Cretaceous and Palaeogene claystones, sandstones and conglomerates. During the latest Cretaceous, Paleocene and Eocene, crustal extension followed by oceanic crust formation took place, causing separation of the continental margins of Greenland and Canada with north-east to northward movement of Greenland. From Paleocene to Eocene, volcanic rocks dominated the central West Greenland continental margin and covered the Cretaceous basins. Development of the oceanic crust is associated with compressional tectonics and the development of strike-slip and thrust faults, pull-apart basins and inversion structures, most pronounced in the Davis Strait and Baffin Bay regions. During the late Cenozoic, tectonism diminished, though some intra-plate vertical adjustments occurred. The latest basin development was characterised by formation of thick Neogene to Quaternary marine successions including contourite drifts and glacial related shelf progradation towards the west and south-west.

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Moon, T., I. Joughin, B. Smith y I. Howat. "21st-Century Evolution of Greenland Outlet Glacier Velocities". Science 336, n.º 6081 (3 de mayo de 2012): 576–78. http://dx.doi.org/10.1126/science.1219985.

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Bergmann, I., G. Ramillien y F. Frappart. "Climate-driven interannual ice mass evolution in Greenland". Global and Planetary Change 82-83 (febrero de 2012): 1–11. http://dx.doi.org/10.1016/j.gloplacha.2011.11.005.

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Cheng, Daniel, Wayne Hayes, Eric Larour, Yara Mohajerani, Michael Wood, Isabella Velicogna y Eric Rignot. "Calving Front Machine (CALFIN): glacial termini dataset and automated deep learning extraction method for Greenland, 1972–2019". Cryosphere 15, n.º 3 (1 de abril de 2021): 1663–75. http://dx.doi.org/10.5194/tc-15-1663-2021.

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Abstract. Sea level contributions from the Greenland Ice Sheet are influenced by the rapid changes in glacial terminus positions. The documentation of these evolving calving front positions, for which satellite imagery forms the basis, is therefore important. However, the manual delineation of these calving fronts is time consuming, which limits the availability of these data across a wide spatial and temporal range. Automated methods face challenges that include the handling of clouds, illumination differences, sea ice mélange, and Landsat 7 scan line corrector errors. To address these needs, we develop the Calving Front Machine (CALFIN), an automated method for extracting calving fronts from satellite images of marine-terminating glaciers, using neural networks. The results are often indistinguishable from manually curated fronts, deviating by on average 86.76 ± 1.43 m from the measured front. Landsat imagery from 1972 to 2019 is used to generate 22 678 calving front lines across 66 Greenlandic glaciers. This improves on the state of the art in terms of the spatiotemporal coverage and accuracy of its outputs and is validated through a comprehensive intercomparison with existing studies. The current implementation offers a new opportunity to explore subseasonal and regional trends on the extent of Greenland's margins and supplies new constraints for simulations of the evolution of the mass balance of the Greenland Ice Sheet and its contributions to future sea level rise.

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van Gool, Jeroen A. M., James N. Connelly, Mogens Marker y Flemming C. Mengel. "The Nagssugtoqidian Orogen of West Greenland: tectonic evolution and regional correlations from a West Greenland perspective". Canadian Journal of Earth Sciences 39, n.º 5 (1 de mayo de 2002): 665–86. http://dx.doi.org/10.1139/e02-027.

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The Nagssugtoqidian Orogen of West Greenland represents a belt of Palaeoproterozoic deformation and metamorphism between the North Atlantic Craton of South Greenland and a northern, lesser known continental segment that includes the Rinkian Orogen. First-order observations are interpreted to support a cycle of separation, convergence, and eventual collision of two continental masses. The emplacement of the Kangâmiut dyke swarm marked the onset of continental breakup at ca. 2040 Ma, and sedimentary basins formed between ca. 1950 and 1920 Ma. Subsequent convergence and consumption of an oceanic plate caused arc magmatism at 19201870 Ma. Granulite-facies peak metamorphism at 18601840 Ma in the centre of the orogen is related to crustal thickening by WNW-directed thrusting. Large-scale, upright folding with an eastwest trend was ongoing by 1825 Ma. Sinistral strike-slip movement was concentrated along steeply dipping limbs of these large-scale folds and formed orogen-scale steep belts at ca. 1775 Ma. Close similarities between the northern and southern foreland suggest that the two cratons likely originated from one continuous continental block. Temporal and kinematic correlation of these events with adjoining orogens in Canada and Greenland shows close genetic links. The Nagssugtoqidian Orogen of West Greenland continues eastwards beneath the Greenland Ice cap to the Eastern Nagssugtoqidian belt of East Greenland (a.k.a. the Ammassalik belt). The Torngat Orogen of eastern Canada developed simultaneous with the Nagssugtoqidian Orogen with a kinematic compatibility suggesting that the two orogens formed on the west and north flanks, respectively, of a curved leading continental margin of an indenting North Atlantic Craton.

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Tesis sobre el tema "Greenland evolution"

White, Arthur Percy 1972. "Extensional evolution of the central East Greenland Caledonides". Thesis, Massachusetts Institute of Technology, 2001. http://hdl.handle.net/1721.1/8233.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2001.
CDROM contains entire thesis in PDF format.
CDROM copy of thesis held by MIT Institute Archives only.
Includes bibliographical references.
This thesis addresses the complexity of both syn- and post-orogenic extension in the overriding plate during Caledonian continental collision through field and laboratory investigations in the central East Greenland Caledonides. During the course of this work, attempts were made to answer some of the outstanding regional and local questions in East Greenland geology. Structural, U-Pb and ⁴⁰Ar/³⁹Ar geochronologic, petrographic and thermobarometric data were combined to constrain and reconstruct a portion of the tectonic history of this orogen. Most extension was accommodated along a system of orogen-parallel, N-S striking normal faults known as the Fjord Region Detachment (FRD) system. The FRD system comprises two temporally distinct, but overlapping, splays just south of 73⁰ N. The lowermost splay is called the Hogedal detachment was active from ca. 417 to 380 Ma, and was active for a second time as recently as ca. 357 Ma. The uppermost splay is the Tindern detachment. This fault was active from ca. 425-423 Ma, exhuming material at rates as fast as 6.5 mm/year. Continued extension in the hanging-wall of this fault accounts for additional denudation at much slower rates over a 25 my time-period. In-between activity on these faults, there is evidence to suggest that middle-crustal thickening continued to occur. Thus, the East Greenland Caledonides preserve evidence for crustal thickening (minimum -16 km) and orogen parallel shear, followed by rapid upper-middle crustal thinning (-13 km), followed by coeval middle-crustal thickening (unknown amount) and upper-crustal thinning (5 km), and ending with crustal collapse (-16 km thinning).
(cont.) This is the first time that an alternation between thrusting and normal faulting has been observed in an over-riding plate during continent-continent collision, and only the second time that it has ever been documented in a collisional orogen. The data imply that there was a fundamental cyclicity between crustal thickening and thinning, consistent with dynamical models of orogenesis in which plate-forces responsible for contraction and gravitational forces responsible for extension, oscillate between periods where one dominates. Furthermore, given the established relationship between topography and synorogenic extension in active mountain belts, it is likely that activity along the Tindern detachment, the earliest splay of the FRD, was controlled by Caledonian paleotopography that formed during the initial stages of orogenesis. The fact that most middle- and upper-crustal extension was restricted to the FRD implies that a localized inherent crustal weakness may have developed after initial movement along the Tindern detachment. Given that late-stage Devonian activity on the FRD may have played a prominent role in the formation of the Devonian basins, which themselves likely controlled the geometry and location of subsequent Mesozoic extension and formation of the North Sea basins, the implication is that the position of rifting of the north Atlantic ocean was partially [pre-determined] inherited from the initial Caledonian paleotopography.
by Arthur P. White.
Ph.D.

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Robertson, S. "Late Archaean crustal evolution in the Ivisartoq region, southern west Greenland". Thesis, University of Exeter, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.353048.

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Stein, Martin. "Evolution and taxonomy of Cambrian arthropods from Greenland and Sweden". Doctoral thesis, Uppsala University, Department of Earth Sciences, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-9301.

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Arthropods have a rich fossil record spanning the Phanerozoic. Biomineralized forms such as the extinct trilobites are particularly common and are proven index fossils for biostratigraphy. Forms with an unmineralized cuticle are more rare, preserved only in so called konservat lagerstätten. Cambrian strata of Greenland have yielded rich trilobite faunas with potential for intercontinental correlation of Cambrian strata, but also an exceptionally preserved fauna, the Sirius Passet Lagerstätte. The first part of this thesis is concerned with trilobite biotratigraphy of the provisional Cambrian Series 2 in Greenland. The second part is concerned with exceptionally preserved arthropods from the Sirius Passet Lagerstätte, but also from 'Orsten' deposits from the Cambrian of Sweden.

Perissopyge phenax occurs in the Henson Gletscher and Paralleldal formations spanning the Series 2 and 3 boundary interval in North Greenland. It also occurs in the Sekwi Formation of Yukon Territory, demonstrating that the species may hold potential for correlation within Laurentia. An indeterminate species of Perissopyge is shown to occur in the Ella Island Formation of North-East Greenland together with Olenellus cf. hanseni, which is similar to Olenellus cf. truemani described from the Henson Gletscher Formation. If this correlation is further corroborated it would offer a first tie-point for the An t'Sron Formation of North-West Scotland which yields Fritzolenellus lapworthi, herein reported for the first time from the Bastion Formation which underlies the Ella Island Formation.

Oelandocaris oelandica from ‘Orsten’ deposits in the Cambrian series 3 and 4 boundary interval in Sweden is an early representative of the Crustacean stem lineage. Kiisortoqia avannaarsuensis is a new arthropod from the Sirius Passet Lagerstätte with robust antennulae strikingly similar to the 'raptorial' limb of the problematic anomalocaridids. The ventral morphology of the 'bivalved' Isoxys volucris is described for the first time and compared with other species assigned to Isoxys from Cambrian lagerstätten around the world. Finally, Siriocaris trolla, is a new arthropod that similarities with trilobites and certain ‘trilobitomorphs’ but seems to lack important synapomorphies of these taxa, though this may be due to preservational limitations in the material at hand.

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Stripp, Gemma Rachel. "The late-stage evolution of the Skaergaard intrusion, East Greenland". Thesis, University of Cambridge, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.608729.

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Martin, Andrew Richard. "The evolution of the Tugtutoq-Ilimaussaq dyke swarm, southwest Greenland". Thesis, University of Edinburgh, 1985. http://hdl.handle.net/1842/12582.

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Alsulami, Sulaiman Lafi. "Tectonic variation and structural evolution of the West Greenland continental margin". Thesis, University of Leeds, 2014. http://etheses.whiterose.ac.uk/7381/.

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The study sets out to unravel the tectonic evolution and lateral structural variation of the West Greenland (Baffin Bay, Davis Strait and Labrador Sea) and to consider its hydrocarbon potential in light of this new evaluation. The study follows a multidisciplinary approach by using 2D seismic, gravity, magnetic, depth-dependent stretching data combined with heat flow and petroleum system modelling. The Western Greenland margin evolved through a complex combination of processes that included multiple phases of extension, varying degrees of subsidence and margin uplift. Basin fill architecture indicates that the margin changes dramatically laterally along the margin. Two rift events were recognized based on architecture of syn-rift sediments. The complex structural variation along the margin is revealed by: the presence of a clear magnetic lineament indicating formation of oceanic crust in Labrador Sea at Chron 31; a good correlation between gravity anomalies in areas of oceanic crust where the extinct spreading axis between Canada and Greenland was identified; areas of continental crust with greater uncertainty in the structure of the continental lithosphere; and greater extension accommodated by the lithosphere in its entirety, rather than by the upper crust alone as indicated by depth-dependent stretching along the margin This study therefore demonstrates that understanding the complex processes involved in multiple-rifting and depth-dependent stretching is important to constraining hydrocarbon potential of passive margin basins.

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Lee, Natasha. "The Neoarchaean tectonothermal evolution of the SE Nuuk region, southern West Greenland". Thesis, University of Edinburgh, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.520515.

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Mader, Marianne M. "From genesis to juxtaposition : the evolution of the Ivisârtoq greenstone belt, southwest Greenland /". Internet access available to MUN users only, 2005. http://collections.mun.ca/u?/theses,64637.

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RiCharde, Gabriel E. "GEOTHERMOBAROMETRIC ANALYSIS AND TECTONIC EVOLUTION OF THE LIVERPOOL LAND ECLOGITES, EAST GREENLAND CALEDONIDES". UKnowledge, 2012. http://uknowledge.uky.edu/ees_etds/10.

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Mineral chemistry and thermobarometry of mafic pods in the Liverpool Land Eclogite Terrane (LLET) provide insight into potential relationships with regional high-pressure (HP) and ultrahigh-pressure (UHP) terranes such as the North East Greenland Eclogite Province (NEGEP), the Western Gneiss Region (WGR), and HP granulites in the East Greenland Caledonides at Payer Land. Grt-cpx thermometry and jadeite barometry performed on garnet and omphacite cores in a sequence of retrogressed eclogites give minimum and average P-T values across six samples for eclogite at 18.4 ± 3.7 kbar at 764 ± 156 °C. Granulite facies conditions based on early retrograde Opx-Plag symplectites, garnet rim compositions, and relict omphacite grains give P-T values at 12.7 ± 0.6 kbar at 860 ± 10 °C, based on grt-cpx thermometry and the opx-grt-pl-qtz equilibra. Late retrograde amphibolite facies conditions, marked by matrix plagioclase and biotite and orthopyroxene symplectite replacement by hornblende symplectites, give mean P-T values of 6.8 ± 0.4 kbar at 740 ± 150 °C, based on grt-cpx thermometry and the grt-hbl-plag-qtz equilibra. Thermometers and barometers yield a qualitative P-T path from lower eclogite facies pressures through the granulite facies via hot isothermal and static decompression, preserving symplectite textures, to amphibolite facies conditions via isobaric cooling. The path is consistent with low-pressure WGR eclogites and suggests affinities between the LLET and Baltica.

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Swientek, Oliver. "The Greenland Norwegian Seaway climatic and cyclic evolution of Late Jurassic-Early Cretaceous sediments /". [S.l. : s.n.], 2002. http://deposit.ddb.de/cgi-bin/dokserv?idn=965036944.

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Libros sobre el tema "Greenland evolution"

Geological history of Greenland: Four billion years of earth evolution. København: Geological Survey of Denmark and Greenland, 2008.

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Upton, B. G. J. Tectono-magmatic evolution of the younger Gardar southern rift, South Greenland. Copenhagen: Geological Survey of Denmark and Greenland, Danish Ministry of Climate, Energy and Building, 2013.

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Huselbee, Maxine Yvonne. Late Cambrian to earliest Ordovician (Ibexian) conodont evolution and biogeography of Greenland and northwest Scotland. Birmingham: University of Birmingham, 1997.

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Pawlowicz, Ryszard A. Tomographic observations of deep convection and the thermal evolution of the Greenland Sea Gyre, 1988-1989. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1994.

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Marienfeld, Peter. Holozäne Sedimentationsentwicklung im Scoresby Sund, Ost-Grönland =: Evolution of sedimentation in Scoresby Sund, East-Greenland during the Holocene. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 1991.

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Garde, Adam A. Accretion and evolution of an Archaean high-grade grey gneiss-amphibolite complex: The Fiskefjord area, southern West Greenland. Copenhagen, Denmark: Geological Survey of Denmark and Greenland, Ministry of Environment and Energy, 1997.

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Tirsgaard, Henrik. Lithostratigraphy, sedimentary evolution, and sequence stratigraphy of the Upper Proterozoic Lyell Land Group (Eleonore Bay Supergroup) of east and north-east Greenland. Copenhagen, Denmark: Geological Survey of Denmark and Greenland, Ministry of Environment and Energy, 1997.

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Schlindwein, Vera. Architecture and evolution of the continental crust of East Greenland from integrated geophysical studies =: Aufbau und Entwicklungsgeschichte der kontinentalen Kruste Ostgrönlands aus integrierten geophysikalischen Untersuchungen. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 1998.

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K, Higgins A., Gilotti Jane A y Smith M. Paul 1959-, eds. The Greenland caledonides: Evolution of the northeast margin of Laurentia. Boulder, Colo: Geological Society of America, 2008.

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Precambrian crustal evolution and Cretaceous-Paleogene faulting in West Greenland. Copenhagen, Denmark: Geological Survey of Denmark and Greenland, Danish Ministry of the Environment, 2006.

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Capítulos de libros sobre el tema "Greenland evolution"

Moorbath, Stephen y Martin J. Whitehouse. "Age of the Isua Supracrustal Sequence of West Greenland: A plausible repository for early life". En Chemical Evolution: Physics of the Origin and Evolution of Life, 87–95. Dordrecht: Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-1712-5_6.

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Snellman, Outi. "The Evolution of Higher Education Collaboration in the Arctic Through Networking". En The Promise of Higher Education, 127–30. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-67245-4_20.

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AbstractAcademic collaboration across the Arctic region—the eight nations bordering the Arctic Circle (United States, Russia, Canada, Denmark/Greenland, Finland, Norway, Sweden and Iceland)—was extremely difficult and restricted during the Cold War years, despite efforts like the establishment of UNESCO and, indeed, the International Association of Universities. Issues and problems, however, do not respect national boundaries: for example, the emergence of massive environmental problems across borders in the region became quite clear during the 1980s. The iron curtain was successful in restricting the movement of people and ideas, but not pollutants.

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Kalsbeek, Feiko y Paul N. Taylor. "Pb-Isotopic Studies of Proterozoic Igneous Rocks, West Greenland, with Implications on the Evolution of the Greenland Shield". En The Deep Proterozoic Crust in the North Atlantic Provinces, 237–45. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5450-2_14.

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Andersen, T., H. Austrheim y D. Bridgwater. "P-T and Fluid Evolution of the Angmagssalik “Charnockite” Complex, SE Greenland". En Fluid Movements — Element Transport and the Composition of the Deep Crust, 71–94. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0991-5_7.

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Herrington, Paul M. y Ian J. Fairchild. "Carbonate shelf and slope fades evolution prior to Vendian glaciation, central East Greenland". En The Caledonide Geology of Scandinavia, 263–73. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2549-6_22.

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Moorbath, Stephen y Balz Samuel Kamber. "Re-Appraisal of the Age of the Oldest Water-Lain Sediments, West Greenland". En Exobiology: Matter, Energy, and Information in the Origin and Evolution of Life in the Universe, 81–86. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-5056-9_7.

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Hambrey, M. J. "The Late Proterozoic sedimentary record of East Greenland: its place in understanding the evolution of the Caledonide Orogen". En The Caledonide Geology of Scandinavia, 257–62. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2549-6_21.

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Nutman, Allen P. y Clark R. L. Friend. "Reappraisal of Crustal Evolution at Kangimut Sammisoq, Ameralik Fjord, Southern West Greenland: Fluid Movement and Interpretation of Pb/Pb Isotopic Data". En Fluid Movements — Element Transport and the Composition of the Deep Crust, 319–29. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0991-5_26.

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Henriksen, Niels, A. K. Higgins, Jane A. Gilotti y M. Paul Smith. "Introduction—The Caledonides of Greenland". En Memoir 202: The Greenland Caledonides: Evolution of the Northeast Margin of Laurentia, v—xv. Geological Society of America, 2008. http://dx.doi.org/10.1130/2008.1202(00).

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Gilotti, Jane A., Kevin A. Jones y Synnøve Elvevold. "Caledonian metamorphic patterns in Greenland". En Memoir 202: The Greenland Caledonides: Evolution of the Northeast Margin of Laurentia, 201–25. Geological Society of America, 2008. http://dx.doi.org/10.1130/2008.1202(08).

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Actas de conferencias sobre el tema "Greenland evolution"

Foulger, Gillian Rose. "EVOLUTION OF THE GREENLAND-ICELAND-FAROES RIDGE". En GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-298332.

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Young, Nicolás E., Gifford Miller, Jason P. Briner, Joerg M. Schaefer, Sarah E. Crump, Alia J. Lesnek y Simon L. Pendleton. "EARLY HOLOCENE EVOLUTION OF THE LAURENTIDE AND GREENLAND ICE SHEETS". En GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297341.

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KROON, AART, JØRN BJARKE TORP PEDERSEN y CHARLOTTE SIGSGAARD. "MORPHODYNAMIC EVOLUTION OF TWO DELTAS IN ARCTIC ENVIRONMENTS, EAST COAST OF GREENLAND". En The Proceedings of the Coastal Sediments 2011. World Scientific Publishing Company, 2011. http://dx.doi.org/10.1142/9789814355537_0172.

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Schiffer, Christian, Stephane Rondenay, Søren Bom Nielsen, Alexander Peace y Scott Jess. "CRUSTAL STRUCTURE OF THE WEST GREENLAND IGNEOUS PROVINCE – IMPLICATIONS FOR TECTONO-MAGMATIC EVOLUTION". En GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357218.

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G. Petersen, T., N. E. Hamann y L. Stemmerik. "Seismic Correlation Increases Understanding of the Paleogene Tectono-stratigraphic Evolution of the North-East Greenland Shelf". En 74th EAGE Conference and Exhibition incorporating EUROPEC 2012. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20148532.

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