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Journal ArticleDOI

Rotations in Lebanon inferred from new palaeomagnetic data and implications for the evolution of the Dead Sea Transform system

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TLDR
In this paper, a study carried out on widespread sites of the Aptian-Albian formations in Lebanon led to two palaeomagnetic directions corresponding to the primary magnetization (N=37 sites, D=307.1°, I=23.7°, k=18 and α95=5.5° after tilt correction and to a post-folding remagnetization).
Abstract
Abstract A study carried out on widespread sites of the Aptian–Albian formations in Lebanon led to two palaeomagnetic directions corresponding to the primary magnetization (N=37 sites, D=307.1°, I=23.7°, k=18 and α95=5.5° after tilt correction and to a post-folding remagnetization (N=18 sites, D=346.3°, I=49.2°, k=108 and α95=3.2° before tilt correction). Comparison of these data with previous palaeomagnetic results for the Jurassic age in Lebanon and expected directions from African apparent polar wander path yields evidence of three different counter-clockwise regional rotations, of the order of 33° before Aptian deposition, of 11° during Late Miocene times, and of 18° since Miocene period. The two last rotations are related to the relative displacement of the African and Arabian plates. A model is proposed for the evolution of this particular Middle East area, in which the Dead Sea Transform shows a strong deviation relative to its main north–south orientation.

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Book ChapterDOI

Lateral Motion and Deformation Along the Dead Sea Transform

TL;DR: In this paper, an updated summary of the history and shallow structure of the Dead Sea transform and its plate tectonic context is presented, where the structures along the DST can be interpreted within the framework of the Sinai-Arabia plate kinematics.
Journal ArticleDOI

Modes and rates of horizontal deformation from rotated river basins: Application to the Dead Sea fault system in Lebanon

TL;DR: In this paper, the authors use the geometry of river basins and numerical modeling to evaluate modes and rates of horizontal deformation associated with the Arabia-Sinai relative plate motion in Lebanon.
Journal ArticleDOI

Transpressive tectonics along a major E-W crustal structure on the Algerian continental margin: Blocks rotations revealed by a paleomagnetic analysis

TL;DR: In this paper, the authors conducted a study on volcanic rocks of Miocene age outcropping on the northern border of the Neogene Chelif basin, northwest Algeria, and found the existence of numerous small tectonic blocks, of probable size around 0.5 to 0.6 kilometers, which underwent clockwise rotations.
Journal ArticleDOI

Tectonic evolution of the central Levant domain (Lebanon) since Mesozoic time

TL;DR: In this article, the tectonic history of the central part of the Levant domain (Lebanon) is re-evaluated and a detailed analysis of the meso-scale brittle deformation is presented.
Book ChapterDOI

Pleistocene Strain Partitioning During Transpression Along the Dead Sea Transform, Metulla Saddle, Northern Israel

TL;DR: The geometry and kinematics of deformation in the Metulla Saddle, a ~4 km-wide and ~9 km-long highly deformed structure across the Dead Sea Transform (DST) between the Hula basin and the Lebanese restraining bend (LRB) is reviewed in this article.
References
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Journal ArticleDOI

Dispersion on a Sphere

TL;DR: In this article, the authors developed a form of theory which appears to be appropriate to measurements of position on a sphere and demonstrated the simultaneous distribution of the amplitude and direction of the vector sum of a number of random unit vectors of given precision.
Journal ArticleDOI

The least-squares line and plane and the analysis of palaeomagnetic data

TL;DR: In this paper, principal component analysis is used to find and estimate the directions of lines and planes of best least squares fit along the demagnetization path of a palaeomagnetic specimen.
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Journal ArticleDOI

Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions

TL;DR: In this article, the optimal recalibration of NUVEL-1 is proposed to multiply the angular velocities by a constant, α, of 0.9562, which is a compromise among slightly different calibrations appropriate for slow, medium, and fast rates of seafloor spreading.
Journal ArticleDOI

On The Geologic Time Scale

TL;DR: GTS2012 as mentioned in this paper summarizes the international divisions and ages in the Geologic Time Scale, published in 2012, since 2004, when GTS2004 was detailed, major developments have taken place that directly bear and have considerable impact on the intricate science of geologic time scaling.
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