Zobrazeno 1 - 10
of 43
pro vyhledávání: '"Hus, R."'
Publikováno v:
In Journal of Structural Geology 2006 28(7):1338-1351
Publikováno v:
In Journal of Structural Geology 2005 27(3):459-473
In recent years, a number of estimates have been proposed of fluctuations of the Baikal lake level caused by climate changes. They were mainly based on the interpretation of reflection seismic data from the Selenga delta area (eastern coast of Lake B
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::fe9b7e41c7db85d0b8300522dbd348f4
http://www.vliz.be/imisdocs/publications/228052.pdf
http://www.vliz.be/imisdocs/publications/228052.pdf
Publikováno v:
%2C+%3Cb%3E%3Ci%3Ein%3C%2Fi%3E%3C%2Fb%3E%3A+Lombardi%2C+S.+%3Ci%3Eet+al.%3C%2Fi%3E+%3Ci%3EAdvances+in+the+geological+storage+of+carbon+dioxide+%E2%80%93+international+approaches+to+reduce+anthropogenic+greenhouse+gas+emissions.+Nato+Science+Series%3A+4.+Earth+and+Environmental+Sciences%2C%3C%2Fi%3E+65%3A+pp.+203-219
Methane, which is at least partly stored in the bottom sediments of Lake Baikal as gas hydrates, is released on the lake floor in the deeper parts of the basin along major faults, forming venting structures similar to small mud volcanoes. The CH4 ven
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::fa99d29e2aa5cd209d5131021b57e2f4
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=210364
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=210364
Scaled physical models constructed with dry sand layers have proven to be a useful tool for the simulation of the structural patterns that are commonly observed in natural rift systems. With this study we have tried to simulate the evolution of the B
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::915f0755a145d204e4c4691087df963a
http://www.vliz.be/imisdocs/publications/228075.pdf
http://www.vliz.be/imisdocs/publications/228075.pdf
The Primorsky Fault is one of the two major western boundary faults in the central part of Lake Baikal. According to the existing fault growth model (e.g. Agar and Klitgord, 1995), this fault has propagated gradually in a southward direction. During
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::282a8138f7bbcea4d9b4a34c40635782
http://www.vliz.be/imisdocs/publications/228196.pdf
http://www.vliz.be/imisdocs/publications/228196.pdf
Natural geological Hg deposits control the Hg levels in the upper Katun river. Very high levels of total Hg are observed in the watercolumn (up to 20 ng L-1) and the sediments (up to 244 µg g-1) close to the deposit area, but almost normal levels (1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::fe7604b86abe8a63618ebd14e2abc18f
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=209150
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=209150
Between the major boundary faults of the central part of Lake Baikal (ie. the Ol’khon fault and the Primorsky fault), a structurally complex tilted area exists that is strongly influenced by the interaction between these two faults. This area, that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::fef4d2ab658bc24d80062cafec6eba16
http://www.vliz.be/imisdocs/publications/228081.pdf
http://www.vliz.be/imisdocs/publications/228081.pdf
The interaction between two offset overlapping normal faults is characterised by the presence of a relay ramp. In order to investigate the way these structures develop, sandbox experiments were carried out. To simulate the brittle crust, we used dry
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::986cdbc6c0e09905ce932830d9242d7e
http://www.vliz.be/imisdocs/publications/228086.pdf
http://www.vliz.be/imisdocs/publications/228086.pdf
The Primorsky range developed along the northwestern side of the Lake Baikal rift basin, at the margin of the Siberian Platform. Morphological investigations revealed that the outlet of Lake Baikal changed several times since the Mid-Pleistocene. Lak
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______232::5f64a4f39de80b52433aa8ad549829ec
http://www.vliz.be/imisdocs/publications/228171.pdf
http://www.vliz.be/imisdocs/publications/228171.pdf