Lineament Characterization and Their Tectonic Significance Using Gravity Data and Field Studies in the Al-Jufr Area, Southeastern Jordan Plateau

Awni Batayneh; Habes Ghrefat; Abdullah Diabat

doi:10.1007/s12583-012-0298-6

Volume 23 Issue 6

Dec 2012

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Journal of Earth Science > 2012 > 23(6): 873-880.

Awni Batayneh, Habes Ghrefat, Abdullah Diabat. Lineament Characterization and Their Tectonic Significance Using Gravity Data and Field Studies in the Al-Jufr Area, Southeastern Jordan Plateau. Journal of Earth Science, 2012, 23(6): 873-880. doi: 10.1007/s12583-012-0298-6

Citation:

Awni Batayneh, Habes Ghrefat, Abdullah Diabat. Lineament Characterization and Their Tectonic Significance Using Gravity Data and Field Studies in the Al-Jufr Area, Southeastern Jordan Plateau. Journal of Earth Science, 2012, 23(6): 873-880. doi: 10.1007/s12583-012-0298-6

Citation:

Awni Batayneh, Habes Ghrefat, Abdullah Diabat. Lineament Characterization and Their Tectonic Significance Using Gravity Data and Field Studies in the Al-Jufr Area, Southeastern Jordan Plateau. Journal of Earth Science, 2012, 23(6): 873-880. doi: 10.1007/s12583-012-0298-6

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Lineament Characterization and Their Tectonic Significance Using Gravity Data and Field Studies in the Al-Jufr Area, Southeastern Jordan Plateau

doi: 10.1007/s12583-012-0298-6

1.
Department of Geology and Geophysics, King Saud University, Riyadh, 11451, Saudi Arabia
2.
Institute of Earth and Environmental Sciences, Al al-Bayt University, Mafraq, Jordan

Funds:

the National Plan for Science, Technology and Innovation (NPST) Program, King Saud University, Saudi Arabia 11-WAT1731-02

More Information

Corresponding author: Awni Batayneh, awni@ksu.edu.sa
Received Date: 10 May 2011
Accepted Date: 08 Sep 2011
Publish Date: 01 Dec 2012

Abstract

Abstract

Lineaments in the southeastern Jordan plateau are mapped using gravity data and field studies in order to understand the tectonic origin of these lineaments, especially in relation to the Dead Sea transform (DST) and the Red Sea opening. Four sets trending E-W, NW-SE, NE-SW, and N-S are identified in gravity data. Field studies generally reveal similar orientations. Field and gravity studies indicate that most of the lineaments are extensional features that correspond to normal faults. Most of these were subsequently reactivated into strike-slip shear fractures. The NW-SE and N-S lineaments represent dilatational fractures. The N-S trending lineaments are the oldest. The E-W lineaments form conjugate shear fractures and are younger than the N-S lineaments. These conjugate shear fractures are also older than other set of conjugate shear fractures oriented NE-SW. The evolution of all these fractures is attributed to the DST and the Red Sea spreading. Kinematic and dynamic analysis of the two, older and younger, pairs of conjugate strike-slip fractures revealed, respectively, broadly NW-SE and N-S oriented transpressional stress (σ₁) with corresponding transtensional stress (σ₃) oriented NE-SW and E-W.
- Jordan plateau,
- gravity data,
- lineament,
- dilatational fracture,
- shear fracture

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References(27)

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