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2011年2月23日，中国科学院特聘研究员，来自挪威水研究所的Thorjørn Larssen博士访问中国科学院地球化学研究所并受邀在环境地球化学国家重点实验室学术报告厅做了精彩的报告。
The Late Riphean Porsangerhalvøyan tectonometamorphic event in the North Norwegian Caledonides:a comment on nomenclature
tectonometamorphic event North Norwegian Caledonides comment nomenclature
2009/12/3
A case is presented for replacing the name 'Porsanger' in 'Porsanger orogeny', in the Kalak Nappe Complex of the Finnmark Caledonides, by the adjectival 'Porsangerhalvøyan'.Moreover, until prov...
Tertiary structure of the Sørkapp-Hornsund Region,South Spitsbergen,and implications for the offshore southern extension of the fold-thrust Belt
Tertiary structure Sø rkapp-Hornsund Region offshore southern extension fold-thrust Belt
2009/12/3
The Sørkapp-Hornsund region of southern Spitsbergen has undergone a complex Tertiary tectonic history, including contractional and transpressional uplift and transtensional subsidence and react...
Mesozoic mudstone compositions and the role of kaolinite weathering–a view from shallow cores in the Norwegian Sea (Møre to Troms)
Mesozoic mudstone compositions kaolinite weathering shallow cores
2009/12/3
Mineralogical data from Mesozoic fine clastic sediments in shallow cores offshore Møre to Troms are compiled. The purpose is to examine stratigraphic and geographic variations in rock compositi...
Sveconorwegian U-Pb zircon and monazite ages of granulite-facies rocks,Hisarøya,Gulen,Western Gneiss Region,Norway
Sveconorwegian U-Pb zircon monazite ages granulite-facies rocks
2009/12/3
U-Pb zircon data from newly discovered granulite-facies rocks on Hisarøya, Gulen,Western Norway, yield a discordia line with upper and lower intercepts of 1646 ± 110 Ma and 987 ± 10 Ma, respect...
The Bjørntvet metabentonite:A new correlation tool for the Silurian of the southwest Oslo Region
Bjø rntvet metabentonite new correlation tool Silurian southwest Oslo Region
2009/12/3
A three-layer horizon of silicate-rich rock exposed in the Bjørntvet limestone quarry in Porsgrunn has been identified as a metabentonite. Its total thickness is 75 cm, it has a dark green-grey...
A re-assessment of the 31st of August 1819 Lurøy earthquake–Not the largest in NW Europe
re-assessment 31st of August 1819 Lurø y earthquake NW Europe
2009/12/3
The Lurøy earthquake of the 31st of August 1819, with magnitude MS = 5.8 – 6.2, is claimed to be the largest in Norway and NW Europe in 'historic' times.We present a re-evaluation of the macros...
Comments on the Lurøy 1819 earthquake controversy
Comments Lurø y 1819 earthquake controversy
2009/12/3
The Lurøy earthquake of 31st August1819 has, for a long time, been rated the largest known earthquake in Norway and in the whole of NW Europe.Recently, Husebye and Kebeasy (2004) published a re...
The 31st of August 1819 Lurøy earthquake revisited
31st of August 1819 Lurø y earthquake
2009/12/3
The 31st of August 1819 Lurøy earthquake has, for a long time, been considered as the largest known historical earthquake in Fennoscandia, possibly even on the mainland of northern Europe. Trig...
Large-scale patterns of glacial streaming flow deduced from satellite imagery over Sør-Trøndelag,Norway
Large-scale patterns glacial streaming flow satellite imagery
2009/12/3
Streamlining features such as drumlinoid forms and glacial striations, deduced from satellite imagery and maps over the Oppdal area, show distinct streamlining patterns that indicate the passage of a ...
The Mesoproterozoic sub-Røynstaul unconformity,central Telemark,Norway
Mesoproterozoic sub-Rø ynstaul unconformity central Telemark
2009/12/3
The traditional Bandak Group of the Mesoproterozoic supracrustal sequences in Telemark, South Norway has recently been subdivided into the Oftefjell (lower) and Høydalsmo groups separated by th...
Fault systems marginal to the Møre-Trøndelag Fault Complex,Osen–Vikna area,Central Norway
Fault systems Mø re-Trø ndelag Fault Complex Osen–Vikna area
2009/12/2
The NE-SW striking Møre-Trøndelag Fault Complex (MTFC) is a key element in the structuring of Mid Norway. Studies of remote sensing data show that the fault complex has a width that exce...
The microfabrics of a porphyroclast-rich quartzitic mylonite,Mjølfjell,Jotun Nappe Complex,Norway
microfabrics porphyroclast-rich quartzitic mylonite Mjø lfjell Jotun Nappe Complex
2009/12/2
This paper describes the microfabrics of a quartzitic mylonite from a shear zone which separates major tectonic units in the Upper Jotun Nappe,a part of the Jotun Nappe Complex. The mylonite is rich i...
Physical and chemical traces of anthropogenic influence at the seabed and in the sediments in Ingøydjupet,Southern Barents Sea
Physical and chemical traces anthropogenic influence sediments
2009/12/2
The MAREANO programme (2006 – 2010) has collected video-footage and surface sediment samples in the Southern Barents Sea during the cruise in 2006. The sampled marine areas included Ingøydjupet...
Transjøen,a Groundwater Influenced Lake with Special Redox and Sulphate Conditions
Groundwater Influenced Lake Special Redox Sulphate Conditions
2009/10/29
Transjeen, a lake in S.E. Norway investigated hydrographically from October
1969 to October 1971, consists of two basins, both of which are meromictic (lake
with lower layer which does not participa...