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Renland

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(a) Cathodoluminescence images showing internal structure of representative...
Published: 01 May 2003
Figure 8. (a) Cathodoluminescence images showing internal structure of representative analysed zircon grains, metapsammite sample no. 452619, Krummedal supracrustal succession, SW Renland. (b) Cathodoluminescence images showing internal structure of representative analysed zircon grains, augen
Journal Article
Published: 01 May 2003
Geological Magazine (2003) 140 (3): 309–333.
...Figure 8. (a) Cathodoluminescence images showing internal structure of representative analysed zircon grains, metapsammite sample no. 452619, Krummedal supracrustal succession, SW Renland. (b) Cathodoluminescence images showing internal structure of representative analysed zircon grains, augen...
FIGURES | View All (14)
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Geological map of the East Greenland Caledonides. <span class="search-highlight">Renland</span> (RL) lies in the ...
Published: 01 May 2003
Figure 1. Geological map of the East Greenland Caledonides. Renland (RL) lies in the Scoresby Sund region within the southern part of the thick-skinned thrust belt. S: Stauning Alper. G: Gasefjord. M: Milne Land. The frame indicates the area of Renland illustrated ° in detail in Figure 4 .
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Large scale recumbent fold structures in paragneisses, Øfjord, SW <span class="search-highlight">Renland</span>. ...
Published: 01 May 2003
Figure 2. Large scale recumbent fold structures in paragneisses, Øfjord, SW Renland. All the thick white sheets are augen granite which mimic the earlier fold structure and are not, in fact, folded (see discussion in text). Highest summit about 1900 m above sea level; for location see Figure 4
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Geological map of southern <span class="search-highlight">Renland</span>, modified after  Chadwick (1975) , to sh...
Published: 01 May 2003
Figure 4. Geological map of southern Renland, modified after Chadwick (1975) , to show localities where the detailed field relationships of the nine tectono-thermal events discussed in the text can be examined in outcrop (numbers 1–9 on inset map, lower left). The tectono-thermal sequence
Image
(a) Cathodoluminescence images showing internal structure of representative...
Published: 01 May 2003
Figure 14. (a) Cathodoluminescence images showing internal structure of representative analysed zircon grains from Caledonian migmatite, sample no. 452640, SE Renland. (b) 207 Pb/ 206 Pb– 238 U/ 206 Pb Tera-Wasserburg plots of zircon and monazite analyses, migmatite sample no. 452640, SE
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(a) Cathodoluminescence images showing internal structure of representative...
Published: 01 May 2003
Figure 12. (a) Cathodoluminescence images showing internal structure of representative analysed zircon grains from granite sheet, sample no. 452651, SW Renland. (b) 207 Pb/ 206 Pb– 238 U/ 206 Pb Tera-Wasserburg plots of zircon analyses, granite sample no. 452651, SW Renland. See text
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(a) Cathodoluminescence images showing internal structure of representative...
Published: 01 May 2003
Figure 11. (a) Cathodoluminescence images showing internal structure of representative analysed zircon grains from garnetiferous aplite vein/patch sample no. 452625, SW Renland. (b) 207 Pb/ 206 Pb– 238 U/ 206 Pb Tera-Wasserburg plots of zircon and monazite analyses, aplite sample no. 452625, SW
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(a) Cathodoluminescence images showing internal structure of representative...
Published: 01 May 2003
Figure 13. (a) Cathodoluminescence images showing internal structure of representative analysed zircon grains from hypersthene monzonite intrusion, sample no. 452635, SE Renland. (b) 207 Pb/ 206 Pb– 238 U/ 206 Pb Tera-Wasserburg plots of zircon analyses, monzonite samples no. 452635
Journal Article
Journal: Geosphere
Published: 25 February 2021
Geosphere (2021) 17 (2): 479–500.
.... The presence of lateral and axial drainage systems is identified and their source regions are constrained. Axial systems are suggested to have likely delivered sediment sourced in East Greenland (Milne Land–Renland) as far south as the south Viking Graben (>800 km). Furthermore, the data highlight...
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Distribution of high temperature granulite facies garnetiferous melt segreg...
Published: 01 May 2003
Figure 7. Distribution of high temperature granulite facies garnetiferous melt segregations constrained by pre-existing folds of compositional layering in the paragneisses, SW Renland. Pencil for scale.
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Intense planar top-to-the-W shear fabric in augen granite cross-cut by garn...
Published: 01 May 2003
Figure 6. Intense planar top-to-the-W shear fabric in augen granite cross-cut by garnetiferous melt segregation during static high temperature granulite facies overprint, SW Renland. Penknife is 10 cm long.
Journal Article
Published: 01 June 1976
Journal of the Geological Society (1976) 132 (3): 289–305.
... 48 21 38 Chadwick, B. 1991 Preliminary account of the geology of south-east Renland, Scoresby Sund, East Greenland. Rapp. Grønlands geol. Unders. 34 , 32 pp. Chadwick, B., 1975. The structure of south Renland, Scoresby Sund, with special reference to the tectono metamorphic evolution...
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Comparison of reconstructed summer sea-surface temperatures (SSTs) from cor...
Published: 01 March 2015
et al., 2011 ); and air temperatures in Greenland derived from the Agassiz and Renland ice core average δ 18 O values, corrected for uplift and changes in δ 18 O content of the ocean ( Vinther et al., 2009 ). Smoothed records (three point running mean) are denoted by bold lines.
Journal Article
Published: 03 October 2011
Geological Magazine (2012) 149 (4): 561–577.
... . 2000 , 2001 ; Kalsbeek, Jones & Jepsen, 2001 ; Kalsbeek, Jones & Nutman, 2001 ; White et al . 2002 ; Leslie & Nutman, 2003 ; Andresen, Rehnström & Holte, 2007 ; Kalsbeek et al . 2008 ). In the very south of the exposed East Greenland Caledonides (in Renland and Milne Land; Fig...
Journal Article
Published: 01 December 2004
Journal of the Geological Society (2004) 161 (6): 1009–1026.
... in Renland (71°15′N; see Fig. 7 ) have yielded slightly younger protolith ages of 915–910 Ma ( Leslie & Nutman 2000, 2003 ). In Renland the augen granites are interpreted to post-date a phase of regional-scale tight to isoclinal folding and upper amphibolite-facies metamorphism affecting the host rocks...
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Journal Article
Journal: Geology
Published: 01 March 2015
Geology (2015) 43 (3): 203–206.
... et al., 2011 ); and air temperatures in Greenland derived from the Agassiz and Renland ice core average δ 18 O values, corrected for uplift and changes in δ 18 O content of the ocean ( Vinther et al., 2009 ). Smoothed records (three point running mean) are denoted by bold lines. ...
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Journal Article
Journal: Geology
Published: 01 November 2007
Geology (2007) 35 (11): 987–990.
.... , and White , J. , 2001 , Oxygen isotope and palaeotemperature records from six Green-land ice-core stations: Camp Century, Dye-3, GRIP, GISP2: Renland and NorthGRIP : Journal of Quaternary Science , v. 16 pp. 299 - 307 doi: 10.1002/jqs.622. Kolstrup , E. , 1980 , Climate...
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Journal Article
Journal: Geology
Published: 01 September 2013
Geology (2013) 41 (9): 1023–1026.
... and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland, and NorthGRIP : Journal of Quaternary Science , v. 16 , p. 299 – 307 , doi:10.1002/jqs.622 . Kawamura K. 17 others , 2007 , Northern Hemisphere forcing of climatic cycles in Antarctica over...
FIGURES
Journal Article
Journal: Geology
Published: 01 February 2010
Geology (2010) 38 (2): 99–102.
... metamorphic analysis of the Westing Group in the Shetland Islands indicates peak metamorphic conditions of 650–700 °C and 0.7 GPa at 950–930 Ma ( Cutts et al., 2009b ). We refer this early Neoproterozoic tectonothermal activity to a Renlandian orogenic event, named after Renland in East Greenland, where...
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