Journal
TECTONOPHYSICS
Volume 721, Issue -, Pages 395-414Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.tecto.2017.10.023
Keywords
Magnetic fabric; Rock-magnetism; AARM; AMS; Magma flow; Dike swarms
Categories
Funding
- FAPESP [2007/56219-0]
Ask authors/readers for more resources
Magnetic fabric and rock magnetism studies were performed on 91 dikes from Cretaceous diabase and lamprophyre dike swarms that outcrop side by side on the beaches of NE Sao Paulo State coastline. The dikes crosscut Archean and Proterozoic poly-metamorphic rocks of the Costeiro Complex. Their thicknesses range from a few centimeters to 2 m for lamprophyre and up to about 10 m for the diabase. They trend predominantly N30 degrees-60 degrees E with vertical dip. Magnetic fabrics were determined using anisotropy of low-field magnetic susceptibility (AMS) and anisotropy of anhysteretic remanent magnetization (AARM). Rock-magnetism measurements reveal that magnetite grains in the range of 2-5 mu m are the magnetic mineral of both swarms. For most dikes, these grains are the carriers of bulk magnetic susceptibility but, surprisingly, are not responsible for the AMS which is carried by Fe-bearing minerals as shown by AARM. The main AMS fabric recognized in the swarms is due to magma flow, in which the K-max-K-int plane is parallel to the dike's plane, and the magnetic foliation pole (K-min) is perpendicular to it. The analysis of the K-max inclination showed that the dikes were fed by horizontal to vertical flows. However, for the majority of the dikes the AMS and AARM tensors are not coaxial. The AARM lineation (AARM(max)) is oriented N30-60W, approximately perpendicular to AMS lineation (K-max) suggesting that magnetite grains were rotated approximately 90 degrees anticlockwise from the dike plane. The AARM(max) orientation is similar to the direction of a fault system mainly in the Santos marginal basin which was formed in the Cretaceous rifting during the South Atlantic opening. Therefore the AARM fabric is tectonic in origin, and the comparison of AMS and AARM fabrics suggests that lamprophyre and diabase dikes were emplaced in three distinct events in the earliest stages of the South Atlantic opening.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available