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CALE Transect C

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Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP460.9
EISBN: 9781786203410
...) . For location of map outline, see Figure 1b . Fig. 1. Index maps. ( a ) Bathymetric and topographic map of the Arctic Ocean and surrounding region showing the location of the Bering Strait CALE Transect C (black line). For details, see Supplementary material, Plate 1. Selected features in ocean...
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Journal Article
Published: 01 September 2010
Journal of Environmental and Engineering Geophysics (2010) 15 (3): 93-110.
...Katherine Grote; Cale Anger; Bridget Kelly; Susan Hubbard; Yoram Rubin Abstract Accurate characterization of near-surface soil water content is vital for guiding agricultural management decisions and for reducing the potential negative environmental impacts of agriculture. Characterizing the near...
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Series: GSA Field Guide
Published: 01 January 2011
DOI: 10.1130/2011.FLD019.09
EISBN: 9780813756196
... root. (A) Starting point of the model, dimensioned according to the retro-deformation of the Sognefjord transect (cf. Fig. 6 , frame 1). (B) Strain distribution when the gravity-driven collapse (ductile rebound) of the orogenic root was almost complete (cf. Fig. 6 , between frames 2 and 3). (C...
Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP460.19
EISBN: 9781786203410
... on the CALE regional sectors ( Fig. 2 ; Sector A, Greenland and Canada; Sector B, Alaska and Chukotka; Sector C, Laptev Sea region; and Sectors E, F and G, Barents/Kara shelf region). The first paper in each section presents the regional integrated onshore–offshore lithospheric-scale transect. Subsequent...
FIGURES
Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP460.12
EISBN: 9781786203410
... as metasedimentary strata. The crystalline crust beneath Segment 3 is the thinnest anywhere on the transect. Both the upper and lower crustal layers are markedly thinner than either to the north or to the south and this is reflected in a Moho that is shallower than elsewhere along the transect, to as little as c...
FIGURES
Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP460.18
EISBN: 9781786203410
... Taimyr (at c. 2200–2300 km in Fig. 8 ). This implies that the lithosphere is stable and still preserves its older structure. In general, the lithosphere-scale structure along Transect 3 shows many similarities to Transects 1 and 2 further south, such as the systematic deepening of the LAB from west...
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Journal Article
Published: 01 February 1993
Journal of the Geological Society (1993) 150 (1): 77-82.
...., INESON, P. R. & MITCHELL, J. G. 1979. The age of mineralization at Parys Mountain, Anglesey. In: HARRIS, A. L., HOLLAND, C. H. & LEAKE, B. E. (eds) Tile Cale&mides of tile British Isles--Reviewed. Geological Society, London, Special Publication, 8, 619 627. O'KEEFE, W. G. 1986. Age and postulated source...
Journal Article
Journal: Geology
Published: 01 October 2009
Geology (2009) 37 (10): 919-922.
...Matthew W. Hughes; Peter C. Almond; Joshua J. Roering Abstract Global sedimentation rates increased during the Quaternary due to frequent landscape adjustment to climatic oscillations. Although high rates of sediment transport are commonly associated with glacial conditions in mountainous terrain...
FIGURES
Journal Article
Published: 01 April 1999
Journal of the Geological Society (1999) 156 (2): 397-410.
...J. J. LOWE; H. H. BIRKS; S. J. BROOKS; G. R. COOPE; D. D. HARKNESS; F. E. MAYLE; C. SHELDRICK; C. S. M. TURNEY; M. J. C. WALKER Abstract The overall aim of the TIGGER IIb project is to increase our understanding of the manner and rates by which ecosystems responded to climate changes during...
Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP460.8
EISBN: 9781786203410
... Island Lithosphere Experiment (ELLITE), carried out in the framework of the Circum Arctic Lithospheric Evolution (CALE) project, provided the first consistent deep seismological transect for the intra-crustal and Moho structure of the Eurekan Orogen on Ellesmere Island ( Fig. 1 ). These data were...
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Journal Article
Journal: GSA Bulletin
Published: 01 September 2007
GSA Bulletin (2007) 119 (9-10): 1218-1231.
... temperatures of zircon and monazite are in excess of 700 °C (e.g., Parrish, 1990 ; Bingen and van Breemen, 1998 ; Montel et al., 2000 ; Cherniak and Watson, 2001 ); thus their ages in amphibolite-grade rocks typically reflect the age of crystallization rather than a cooling age. However, because several...
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Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP460.2
EISBN: 9781786203410
... Formation; D 2-3 gt, Gureytyvis Formation; D 3 vt, Varkatyvis Formation; C 1 vz, Vazhhanovey Formation; C 1 br1/2, Buredan Formation lower/upper. Fig. 8. Structural data from a transect across the Main Pai-Khoi Thrust, Silova River, SE Pai-Khoi. ( a ) Poles to bedding preserved in the hanging...
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Journal Article
Journal: Geology
Published: 01 May 2008
Geology (2008) 36 (5): 379-382.
.... Data from the new site suggest that patterns of climatological change were similar across a meridional transect of western North America but that PETM climate was relatively more arid in the southern Rocky Mountains, possibly reflecting diversion of precipitation from middle to high latitudes. Our...
FIGURES
Series: SEPM Special Publication
Published: 01 January 2000
DOI: 10.2110/pec.00.66.0349
EISBN: 9781565761889
...). Enthusiastic field assistance by N. Van Wyck was absolutely critical to work completed during the summer of 1986. We thank J. Amato and J. Fournelle at the University of Wisconsin for performing microprobe analyses of the organic-rich dolomite. Very helpful discussions were held with L. C. Pray, T. Simo, G. B...
Journal Article
Journal: Geosphere
Published: 05 December 2019
Geosphere (2019)
..., and intermittent magmatism in response to right-oblique oceanic-continental plate convergence (Farallon–North America). High-strain linear-planar tectonite fabrics are recorded along an unbroken ~48 km west-to-east transect extending from the Snake River (Wallowa intra-oceanic arc terrane; eastern Blue Mountains...
Journal Article
Published: 20 October 2016
Journal of the Geological Society (2017) 174 (1): 75-87.
...Penelope J. Lancaster; J. Stephen Daly; Craig D. Storey; Andrew C. Morton Abstract Establishing the source(s) of sedimentary material is critical to many geological applications, but is complicated by the ability of some minerals to be recycled. To test the relative utility of current proxies...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2008
GSA Bulletin (2008) 120 (5-6): 659-678.
...Linda C. Ivany; Kyger C. Lohmann; Franciszek Hasiuk; Daniel B. Blake; Alexander Glass; Richard B. Aronson; Ryan M. Moody Abstract A high-resolution record of Eocene paleo-temperature variation is preserved within the high southern latitude, marine shelf succession of the La Meseta Formation...
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Journal Article
Journal: GSA Bulletin
Published: 19 December 2017
GSA Bulletin (2018) 130 (5-6): 825-847.
... of diagenesis ( Fig. 4C ). Figure 4. Photomicrographs of three sediment types from the Kobuk Koyukuk subbasin. (A) Type 1 sediment with characteristic chert lithic and monocrystalline plagioclase (Ca-rich) grains. (B) Volcanic lithic in type 1 sandstone unit. (C) Gabbroic lithic in type 1 sandstone. (D...
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Journal Article
Journal: Geology
Published: 01 May 2009
Geology (2009) 37 (5): 451-454.
...Atsushi Ando; Brian T. Huber; Kenneth G. MacLeod; Tomoko Ohta; Boo-Keun Khim Abstract Detailed multitaxon stable isotope (δ 18 O and δ 13 C) data from Blake Nose (western North Atlantic) argue against a mid-Cenomanian glaciation event during the mid-Cretaceous greenhouse. Results generated...
FIGURES
Journal Article
Published: 01 July 1977
Journal of the Geological Society (1977) 133 (5): 413-432.
..., Ireland; their structural compartmentation and place in the Caledonian orogen C. B. LONG & M. D. MAX SUM Three tectono-sedimentary units having Cale- donian tectono-thermal histories are recognized within the metamorphic rocks of the SW Ox Mountains Inlier. The different structural levels represented...