1-20 OF 74 RESULTS FOR

Suhre Valley

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Image
Map (<b>Suhre</b> <b>Valley</b>) showing the locations of the shallow 3-D seismic reflect...
in > Geophysics
Published: 01 January 2001
F IG . 1. Map (Suhre Valley) showing the locations of the shallow 3-D seismic reflection survey area (boxed region) and two intersecting pilot 2-D seismic profiles (numbered 1 and 2) from Büker et al. (1998a) . Borehole locations are numbered I-III. Survey site within northern Switzerland
Image
Map of survey area (<b>Suhre</b> <b>valley</b>) showing 3-D seismic reflection site (boxe...
in > Geophysics
Published: 01 January 2000
F IG . 1. Map of survey area (Suhre valley) showing 3-D seismic reflection site (boxed area) and two intersecting 2-D seismic profiles (-1- and -2-) presented by Büker et al. (1998a) . Two boreholes are numbered I and II. Stippled pattern outlines glacial moraines, light grey represents exposed
Journal Article
Journal: Geophysics
Published: 01 August 1998
Geophysics (1998) 63 (4): 1395-1407.
...Frank Bueker; Alan G. Green; Heinrich Horstmeyer Abstract Shallow seismic reflection data were recorded along two long (>1.6 km) intersecting profiles in the glaciated Suhre Valley of northern Switzerland. Appropriate choice of source and receiver parameters resulted in a highfold (36-48) data...
Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP446.4
EISBN: 978-1-78620-376-2
... time. Compaction continues in post-eruptive time and may be accompanied by mineral reactions resulting from the presence of groundwater and different rock types, i.e. juvenile and various accidental clast types ( Lorenz et al. 2003 ; Suhr et al. 2006 ). In the case of the large diatremes...
FIGURES | View All (10)
Image
Location of survey areas in northern Switzerland. (a) Rhine <b>valley</b>. Coincid...
in > Geophysics
Published: 01 January 2001
). Highlighted area shows location of previously recorded shallow 3-D seismic reflection survey (R. Spitzer, F. Nitsche and A. Green, in preparation). (b) Suhre valley. Coincident seismic reflection profiles with different types of geophones were recorded along a gravel track (solid line). Highlighted area shows
Journal Article
Journal: GSA Bulletin
Published: 01 January 2006
GSA Bulletin (2006) 118 (1-2): 94-108.
... Cove terrane in northern Quebec. It has long been known that similarly ancient gneisses are exposed on the southern margin of the Superior craton in the Minnesota River Valley and in northern Michigan, but the ages of these rocks have been poorly constrained, because methods applied in the 1960s...
FIGURES | View All (14)
Image
Stacked sections recorded simultaneously along compacted gravel track in th...
in > Geophysics
Published: 01 January 2001
F IG . 17. Stacked sections recorded simultaneously along compacted gravel track in the Suhre valley with (a) towed land streamer and (b) spike-mounted geophones. (c) Difference between stacked sections (b) and (a). Amplitude scaling of three sections is identical. Processing sequence shown
Journal Article
Journal: Geophysics
Published: 01 January 2000
Geophysics (2000) 65 (1): 18-34.
...F IG . 1. Map of survey area (Suhre valley) showing 3-D seismic reflection site (boxed area) and two intersecting 2-D seismic profiles (-1- and -2-) presented by Büker et al. (1998a) . Two boreholes are numbered I and II. Stippled pattern outlines glacial moraines, light grey represents exposed...
FIGURES | View All (16)
Journal Article
Published: 20 February 2003
Canadian Journal of Earth Sciences (2003) 40 (2): 207-219.
... fault. The Oak Hill Group was deposited near a triple-rift zone. Clastic sediments of this group formed a large delta that was fed by a major river flowing in the rift valley of the Ottawa graben. The delta must have prograded on a gentle slope platform. No other thick deltaic deposits are known towards...
FIGURES | View All (5)
Series: Geological Society, London, Special Publications
Published: 01 January 2015
DOI: 10.1144/SP393.1
EISBN: 9781862396692
... settings are tied to plate margin processes (e.g. orogenic gold, volcanic-hosted massive sulphide, Mississippi valley type Pb–Zn deposits) correlates well with the supercontinent cycle, whereas deposits related to intra-cratonic settings and mantle-driven igneous events, such as Ni–Cu–PGE deposits, lack...
FIGURES | View All (5)
Journal Article
Published: 01 September 1997
Journal of the Geological Society (1997) 154 (5): 829-838.
.... The Clew Bay and Highland Border Complexes, both being parts of the Border Terrane, have many similarities including evidence of mid- to late Ordovician spreading, and it is suggested they formed in the same basin. However, they are dissimilar to both the South Mayo and Midland Valley Ordovician...
Series: GSA Memoirs
Published: 01 January 2008
DOI: 10.1130/2008.1202(06)
.... In the Franklinian Basin of eastern North Greenland, unconformity-bounded Lower Cambrian sediments can be correlated with the Sauk I sequence of cratonic North America. These Cambrian sediments are separated from younger units by a significant hiatus, the sub–Wandel Valley unconformity, but above that surface...
FIGURES | View All (14)
Journal Article
Journal: Geophysics
Published: 01 January 2001
Geophysics (2001) 66 (6): 1761-1773.
...F IG . 1. Map (Suhre Valley) showing the locations of the shallow 3-D seismic reflection survey area (boxed region) and two intersecting pilot 2-D seismic profiles (numbered 1 and 2) from Büker et al. (1998a) . Borehole locations are numbered I-III. Survey site within northern Switzerland...
FIGURES | View All (13)
Journal Article
Journal: Geophysics
Published: 01 January 2001
Geophysics (2001) 66 (2): 482-500.
...). Highlighted area shows location of previously recorded shallow 3-D seismic reflection survey (R. Spitzer, F. Nitsche and A. Green, in preparation). (b) Suhre valley. Coincident seismic reflection profiles with different types of geophones were recorded along a gravel track (solid line). Highlighted area shows...
FIGURES | View All (22)
Journal Article
Journal: GSA Bulletin
Published: 01 August 2001
GSA Bulletin (2001) 113 (8): 1025-1038.
...Günter Suhr; Peter A. Cawood Abstract The Lewis Hills massif (Bay of Islands Ophiolite, Newfoundland) preserves a deeply eroded transform fault. A major, low-angle, extensional mylonite zone is next to the transform assemblage and probably merges laterally into it. The mylonite developed in a high...
FIGURES | View All (10)
Journal Article
Journal: PALAIOS
Published: 24 July 2018
PALAIOS (2018) 33 (7): 312-322.
... , 1875 ; Velenovský 1885 ; Frič 1889 , 1893 ). Later, Bather (1911) interpreted it as the tube of terebelloid polychaetes ascribed to Terebella . This idea was followed by Häntzschel (1931) , Abel (1935) , and Fuchs (1935) , and confirmed by Suhr (1988) , who transferred Cunninghamites...
FIGURES | View All (8)
Journal Article
Journal: Geology
Published: 01 February 2016
Geology (2016) 44 (2): 167-170.
...) deployed at the southernmost area of the Central Indian Ridge (sample location is shown in the GSA Data Repository 1 ). The peridotites were sampled at the Yokoniwa Rise, a mantle outcrop located at the eastern valley wall of the Central Indian Ridge axis. We selected four peridotites, consisting...
FIGURES | View All (4)
Journal Article
Published: 01 September 2006
Journal of the Geological Society (2006) 163 (5): 869-879.
... and troctolite (D-T) shown in ( e ). We sampled present-day sandy sediments at eight localities in wadis (valleys), which have only mantle section exposed upstream (i.e. near the base of the Moho transition zone) in the northern Oman ophiolite ( Fig. 1 ). We define the base of the Moho transition zone...
FIGURES | View All (9)
Journal Article
Journal: Geosphere
Published: 01 February 2017
Geosphere (2017) 13 (1): 136-154.
... undeformed ( Fig. 4B ), such as in a typical root zone of diabase dikes complex. It is along the western foothills of Krabbi and Puka massifs that an undeformed crustal unit is exposed extending along the Dedaj Valley ( Fig. 2 ). These lowlands are occupied by highly altered gabbros ( Figs. 5A and 5B...
FIGURES | View All (11)
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1976
AAPG Bulletin (1976) 60 (6): 952-961.
... of the Doonerak anticline Mississippian rocks overlie the Cambrian or Ordovician rocks with angular unconformity ( Brosge et al, 1974 ), and are overlain in turn by Pennsylvanian, Permian, and Triassic rocks. Just across the valley on the north, the normal thick Upper Devonian clastic sequence of the north...
FIGURES | View All (5)