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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Aar Valley (1)
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Africa
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East Africa
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Tanzania
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Oldoinyo Lengai (1)
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Australasia
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Russian Federation
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Europe
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Alps
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Western Alps
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Brianconnais Zone (3)
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Germany
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volcanic rocks
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rutile (3)
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tellurides (2)
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Primary terms
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absolute age (13)
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Africa
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Tanzania
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Oldoinyo Lengai (1)
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-
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North Africa (1)
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Antarctica
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Asia
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Kazakhstan
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Far East
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Japan (1)
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Middle East
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Iran (1)
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Turkey (1)
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Tuva Russian Federation (1)
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Atlantic Ocean
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North Atlantic
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North Sea
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Viking Graben (1)
-
-
-
-
Australasia
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Australia
-
New South Wales Australia (1)
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South Australia
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Flinders Ranges (1)
-
-
-
New Zealand
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-
-
-
bacteria (2)
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biography (1)
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Canada
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Eastern Canada
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Nunavut
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Ellesmere Island (1)
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Western Canada
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Alberta (1)
-
-
-
carbon
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organic carbon (1)
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Cenozoic
-
Quaternary
-
Holocene
-
lower Holocene (1)
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Neoglacial (2)
-
-
upper Quaternary (2)
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-
Tertiary
-
middle Tertiary (2)
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Neogene
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Miocene
-
lower Miocene
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Burdigalian (1)
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-
-
Pliocene (1)
-
-
Paleogene
-
Eocene
-
upper Eocene (1)
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-
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clay mineralogy (1)
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climate change (5)
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Europe
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Alps
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Bernese Alps (9)
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Lepontine Alps (2)
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Pennine Alps (28)
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-
Eastern Alps
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Hohe Tauern (1)
-
-
French Alps (5)
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Limestone Alps (1)
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Piedmont Alps
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Dora Maira Massif (1)
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Prealps (4)
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South Austrian Alps (1)
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Swiss Alps
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Central Swiss Alps (5)
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Northern Swiss Alps (1)
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Southern Swiss Alps (14)
-
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Western Alps
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Cottian Alps
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Dora Maira Massif (1)
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Dauphine Alps
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Belledonne Massif (1)
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Maritime Alps (1)
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Mont Blanc (5)
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Savoy Alps (2)
-
-
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Brianconnais Zone (3)
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Carpathians
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Western Carpathians (1)
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Central Europe
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Austria
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Styria Austria (1)
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Black Forest (1)
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Germany
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Molasse Basin (2)
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Aar Massif (4)
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Bern Switzerland
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Grimsel Test Site (6)
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Bernese Alps (9)
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Southern Swiss Alps (14)
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Ticino Switzerland (1)
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Valais Switzerland
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Binnental (29)
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Zermatt Switzerland (7)
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Vaud Switzerland (1)
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Pyrenees
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Italy
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Ivrea Italy (1)
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GITEC: A Generalized Inversion Technique Benchmark
Tennantite-(Hg), Cu 6 (Cu 4 Hg 2 )As 4 S 13 , a new tetrahedrite-group mineral from the Lengenbach quarry, Binn, Switzerland
Time-lapse ground penetrating radar difference reflection imaging of saline tracer flow in fractured rock
Temporal variations in rockfall and rock-wall retreat rates in a deglaciated valley over the past 11 k.y.
Postglacial erosion of bedrock surfaces and deglaciation timing: New insights from the Mont Blanc massif (western Alps)
Gasparite-(La), La(AsO 4 ), a new mineral from Mn ores of the Ushkatyn-III deposit, Central Kazakhstan, and metamorphic rocks of the Wanni glacier, Switzerland
Abstract Geological disposal is the most realistic option for high-level radioactive waste in Japan. In considering long-term stability for geological disposal, several types of materials have been studied as engineered barriers with a host rock. We focused our study on metal and bentonite as engineered barrier materials and investigated the long-term corrosion tendency of the metal exposed to bentonite. An electrochemical method for inducing accelerated corrosion was studied in a laboratory, and we analysed some field samples from a FEBEX dismantling project (FEBEX-DP) in Switzerland for comparison with our experimental results.
Penetration depth of meteoric water in orogenic geothermal systems
Interpretation pitfalls to avoid in void interpretation from ground-penetrating radar imaging
Large vertical displacements of a crystalline massif recorded by Raman thermometry
New data on cafarsite: reinvestigation of its crystal structure and chemical composition
UHP Ti-chondrodite in the Zermatt-Saas serpentinite: Constraints on a new tectonic scenario
Structural and metamorphic evolution during tectonic mixing: is the Rocca Canavese Thrust Sheet (Italian Western Alps) a subduction-related mélange?
Detection of Weak Seismic Signals in Noisy Environments from Unfiltered, Continuous Passive Seismic Recordings
Ni-serpentine nanoflakes in the garnierite ore from Campello Monti (Strona Valley, Italy): Népouite with some pecoraite outlines and the processing of Ni-containing ore bodies
Abstract Deep-water conglomeratic megabeds are recognized in the Upper Jurassic Brae member (equivalent to part of the more regionally defined Brae Formation) of the Kimmeridge Clay Formation in UK Block 16/17, within the South Viking Graben in several submarine fans, but have not been described in detail previously. The megabeds are distinguished from enveloping turbidite beds by their fabrics, their scale, and their clast composition. They are distinguished from mass-transport deposits (MTDs), slumps, and slides by being predominantly conglomeratic. The conglomeratic megabeds are compared with a series of conglomeratic megabeds from the Cerro Toro Formation of the Magallanes Basin, southern Chile, with megabeds from eastern Turkey, and with other well-known megabeds from around the world. The megabeds are interpreted as event beds that (1) occur randomly in the stratigraphy and are inferred to have been triggered by seismic events, (2) occur at the initiation of channel complex development, or (3) occur due to sea-level fall and are found at the base of large-scale fining-upward conglomeratic deep-water fans. Though many of the Brae member megabeds are clast-supported and disorganized, and interpreted as the product of avalanche scree from the basin-bounding fault escarpment into deeper water, some have more complex fabric indicating flow transformation. The Cerro Toro megabeds are predominantly more organized, ideally with tripartite or bipartite fabric, though divisions vary widely in occurrence, thickness, and composition. These lithofabrics are interpreted as the product of different flow rheologies that changed in time and space, reflecting flow transformation. The tripartite megabeds are here called transitional event deposits, or TEDs. Division 1 is preceded by erosion and the development of large flute marks, implying that the initial phase of a TED was a turbidity current. The lower part of Division 1 has a thin, clast-supported granular lag with a wavy top followed by a thicker, clast-supported interval with up to boulder-grade extrabasinal clasts and a coarse-granular, less than 10% sandstone matrix. This is interpreted as the deposit of a high-density turbidity current that largely bypassed at this point, leaving disorganized to weakly stratified and locally imbricated conglomerate. Division 2 is transitional with Division 1 over tens of centimeters (several inches) into a progressively more matrix-supported pebbly sandstone. The lower interval of Division 2 has an approximately 50% clast content, 50% coarse-grained sandstone matrix, and an increasing prevalence of mud clasts upward. The mud clasts increase in diameter and angularity upward, with a normal grading of lithic clasts and a gradual upward fining of the matrix. The upper interval of Division 2 is generally poor in extrabasinal clasts, but with an increase in rafted sandstone blocks as well as heterolithic clasts, and also a gradual increase in clay in the matrix. Some of the TEDs have a structureless mud cap with rare floating pebbles. Rafted intrabasinal sandstone clasts are particularly common in the Cerro Toro Formation TEDs and are also recognized in the Brae member. Division 2 is interpreted as the product of a debris flow, within which there has been significant grain size segregation. Division 2 marks rapid flow transformation and the development of a rigid plug as the event rapidly decelerated. Division 3, where present, is a structureless dirty sandstone, with mud chips, that thickens and thins and often pinches out, over the topographically irregular, sandstone block-rich, top to Division 2. It may be transitional with Division 2 but is much more commonly sharp, or even erosive, into it. Division 3 may have a sharp or graded top, sometimes fining to claystone, though the preservation potential for this is low. Division 3 is interpreted as a co-genetic turbidite. The TEDs form one end-member family of a range of megabeds, representing complex large-scale events that were sustained for periods that allow the flows to evolve in time and space, reflecting a progressive collapse of the feeder system in a repeatable manner. A scheme documenting the range of these thick deep-water conglomeratic event beds is proposed. Most of these events are best understood in the context of a fan delta clinoform prograding during river flood onto a muddy deep-water slope and headward-eroding scars on the retrogressive collapse front going through a series of steps that generate a range of events, from simple submarine scree avalanches such as those seen in the Brae systems through to events that changed and transformed during transport to produce complicated tripartite event beds such as a TED.