International Journal of Earth Sciences
Công bố khoa học tiêu biểu
* Dữ liệu chỉ mang tính chất tham khảo
Sắp xếp:
Glacial–interglacial records of the reflectance of sediments from the Norwegian–Greenland–Iceland Sea (Nordic seas)
International Journal of Earth Sciences - Tập 88 - Trang 325-336 - 1999
The reflectance of sediments (gray level) were measured on 11 sediment cores from the Norwegian–Greenland–Iceland Sea (Nordic seas). The analyzed time interval covers the past five glacial–interglacial cycles. Although the results demonstrate that the gray-level method has a potential for stratigraphic purposes, it is indicated that gray-level changes in the Nordic seas are not necessarily driven...... hiện toàn bộ
Does AMS data from micaceous quartzite provide information about shape of the strain ellipsoid?
International Journal of Earth Sciences - Tập 101 - Trang 693-703 - 2011
Anisotropy of magnetic susceptibility (AMS) in micaceous quartzites with mean susceptibility (K
m) >50 × 10−6 SI units is known to be on account of the orientation distribution of the para/ferromagnetic minerals (e.g. micas, magnetite), which comprise the minor phase in the rocks. However, the strain in such deformed micaceous quartzites is dominantly accommodated by the quartz gra...... hiện toàn bộ
Evolution of sedimentary basins — the integrated modeling approach
International Journal of Earth Sciences - - 1989
Sr–Nd isotope and geochemical characterisation of the Paleoproterozoic Västervik formation (Baltic Shield, SE-Sweden): a southerly exposure of Svecofennian metasiliciclastic sediments
International Journal of Earth Sciences - Tập 101 Số 1 - Trang 39-55 - 2012
The Paleoproterozoic Västervik formation represents the southernmost exposure of Svecofennian metasediments and comprises a large psammitic succession of up to 5,000 m thickness dominated by quartzite with minor pelite and arkose. The Västervik formation was deposited in a time interval of ~30 m.y. from 1.88 until 1.85 Ga. Whole-rock geochemical data and Rb–Sr–Sm–Nd analyses in comb...... hiện toàn bộ
Fault damage zone origin of the Teufelsmauer, Subhercynian Cretaceous Basin, Germany
International Journal of Earth Sciences - Tập 102 - Trang 121-138 - 2012
Recognition of fractures as porosity-reducing deformation bands pervading all sandstone segments of the Teufelsmauer, Subhercynian Creatceous Basin, Germany, motivates a study relating the observed macroscopic and microscopic deformation to the damage zone of the nearby Harz border fault. Deformation bands, confirmed and documented by several porosity-reducing micro-mechanisms, such as cataclasis,...... hiện toàn bộ
Structural model of the Balkassar area, Potwar Plateau, Pakistan
International Journal of Earth Sciences - - 2015
Support for the Giant Wave Hypothesis: evidence from submerged terraces off Lanai, Hawaii
International Journal of Earth Sciences - Tập 96 - Trang 517-524 - 2006
The origin of subaerial coral conglomerate deposits on the Hawaiian islands of Lanai and Molokai is controversial, primarily because these deposits are difficult to interpret and the vertical motion of these islands is poorly constrained. Based on bathymetry, dive observations, sedimentary and radiocarbon data from coralline algal dominated deposits from two submerged terraces at −150 and −230 m o...... hiện toàn bộ
The growth, collapse and quiescence of Teno volcano, Tenerife: new constraints from paleomagnetic data
International Journal of Earth Sciences - Tập 95 - Trang 1053-1064 - 2006
Tenerife basically consists of three Miocene shield volcanoes, the Anaga, the Teno and Central shield, as well as the Pliocene Cañadas volcano. The temporal evolution and structural significance of each volcano with respect to the history of Tenerife is still a matter of debate. We present paleomagnetic results in order to enhance the view of the volcanic history of the Teno volcano by means of ma...... hiện toàn bộ
Structural development of the central Kyrenia Range (north Cyprus) in its regional setting in the eastern Mediterranean region
International Journal of Earth Sciences - Tập 105 - Trang 417-437 - 2015
A detailed structural analysis of the Mesozoic–Cenozoic geological development of the central segment of the Kyrenia Range in its regional tectonic context is given here. The structural evidence comes from five structural traverses, outcrop observations, small-scale structures and related regional evidence. The majority of the structures are fault planes, of which a subordinate number exhibit slic...... hiện toàn bộ
The Variscan tectonic inheritance of the Upper Rhine Graben: evidence of reactivations in the Lias, Late Eocene–Oligocene up to the recent
International Journal of Earth Sciences - - 2007
Tổng số: 2,021
- 1
- 2
- 3
- 4
- 5
- 6
- 10