Zobrazeno 1 - 10
of 44
pro vyhledávání: '"H.-U. Worm"'
Autor:
H.-U. Worm
Publikováno v:
Earth and Planetary Science Letters. 193:287-302
Ocean Drilling Program (ODP) Hole 735B was drilled to a depth of 1.5 km in a tectonic window of gabbroic lower oceanic crust created at the Southwest Indian Ridge. The gabbros have a very stable natural remanent magnetization (NRM) of reversed polari
Publikováno v:
Terra Nova. 10:211-216
Using recently acquired marine magnetic data and existing magnetic and bathymetric data sets together with ODP Leg 170 age determinations we present a revised plate tectonic model for the southern Cocos and northern Nazca plate area. According to thi
Publikováno v:
Geophysical Journal International. 114:127-137
Summary The field and frequency dependences of the initial susceptibility of pyrrhotite have been analysed as a function of grain size, motivated by a strong field dependence recently observed for large (mm-sized) pyrrhotite crystals (Worm 1991) and
Autor:
H.-U. Worm, Subir K. Banerjee
Publikováno v:
Geophysical Journal International. 102:359-364
SUMMARY Multidomain ferro- and ferrimagnets carrying a thermoremanent magnetization (TRM) display a maximum in remanent magnetization just below the Curie temperature Tc when continuously demagnetized in zero field. We interpret this demagnetization
Autor:
H. J. B. Dick, J. H. Natland, D. J. Miller, J. C. Alt, W. Bach, D. Bideau, J. S. Gee, S. Haggas, J. G. H. Hertogen, G. Hirth, P. M. Holm, B. Ildefonse, G. J. Iturrino, B. E. John, D. S. Kelley, E. Kikawa, A. Kingdon, P. J. Le Roux, J. Maeda, P. S. Meyer, H. R. Naslund, Y. Niu, P. T. Robinson, J. E. Snow, R. A. Stephen, P. W. Trimby, H.-U. Worm, A. Yoshinobu
Publikováno v:
Proceedings of the Ocean Drilling Program : Initial reports
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::93724a6bed8f961dc134f0541c699896
https://gfzpublic.gfz-potsdam.de/pubman/item/item_227721
https://gfzpublic.gfz-potsdam.de/pubman/item/item_227721
Publikováno v:
Geology. 26:487
A 4.3-km-thick section of clastic sediments of the Surma basin, northeastern Bangladesh, that is exposed along the Shari River was sampled for a magnetostratigraphic study. Miocene through Pleistocene ages have been discussed previously; however, the