Data report; Reorientation of structural features at sites 920 to 924 using remanent magnetization and magnetic characteristics

Citation:
Hurst, SD, Gee JS, Lawrence RM.  1997.  Data report; Reorientation of structural features at sites 920 to 924 using remanent magnetization and magnetic characteristics. Proceedings of the Ocean Drilling Program, Scientific Results. 153:547-559.

Keywords:

12, Stratigraphy, Atlantic Ocean, boundary conditions, Brunhes Chron, Cenozoic, gabbros, igneous rocks, Kane fracture zone, Koenigsberger ratio, Leg 153, magnetic anomalies, magnetite, magnetization, Matuyama Chron, mid-atlantic ridge, natural remanent magnetization, North Atlantic, Ocean Drilling Program, oxides, paleomagnetism, plutonic rocks, Quaternary, remanent magnetization, upper Cenozoic, upper Quaternary

Abstract:

Drilling at Ocean Drilling Program Sites 920 to 924 recovered core with a diverse set of pervasive structural elements. Site 920 recovered predominantly peridotitic rocks that display an early crystal-plastic fabric overprinted by at least five generations of veins. Sites 921 to 924 recovered gabbros that contain magmatic and metamorphic foliations and lineations developed to varying intensities throughout. Brittle features in the gabbro core include Cataclastic zones, faults, and several generations of veins. The characteristic magnetization direction was used to estimate the in situ orientation of structural features within the core. Although significant uncertainty is associated with the unknown effects of anisotropy and tectonic rotations on the rema- nent declinations, the corrected attitudes of the dominant foliations at Site 920 dip gently east-northeast, parallel to other obser- vations of seafloor structures in the area. Other vein generations and structural features in the rocks do not have a consistent orientation with respect to each other or a consistent variation with core depth. Sites 921-924 were drilled into a section of mostly gabbroic rocks that typically have complicated magnetic properties, with several remanence components identifiable during demagnetization. Reorientation of the gabbro cores is less certain because of the complexity of the remanent magnetiza- tion components, however, many structures in the gabbro from Hole 923A also seem to have gentle dips to the northeast after such a reorientation.

Notes:

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DOI:

10.2973/odp.proc.sr.153.040.1997