Indication Strike Slip Movement A Part of Sorong Fault Zone in Yapen Island, Papua, Indonesia

2014 ◽  
Author(s):  
Fahmi Ikhwanudin ◽  
Chalid Idham Abdullah
Keyword(s):  
Fault Zone ◽  
Strike Slip ◽  
Strike Slip Movement

40Ar/39 Ar geochronological constraints on syn-orogenic strike-slip movement of Tan-Lu fault zone

2004 ◽  
Vol 49 (5) ◽  
pp. 499-508 ◽  
Author(s):  
Guang Zhu ◽  
Guosheng Liu ◽  
W. J. Dunlap ◽  
C. Teyssier ◽  
Yongsheng Wang ◽  
...  
Keyword(s):  
Fault Zone ◽  
Strike Slip ◽  
Geochronological Constraints ◽  
Strike Slip Movement

Geological analysis and FT dating of the large-scale right-lateral strike-slip movement of the Red River fault zone

2007 ◽  
Vol 50 (3) ◽  
pp. 331-342 ◽  
Author(s):  
HongFa Xiang ◽  
JingLin Wan ◽  
ZhuJun Han ◽  
ShunMin Guo ◽  
WanXia Zhang ◽  
...  
Keyword(s):  
Fault Zone ◽  
Large Scale ◽  
Strike Slip ◽  
Red River ◽  
Lateral Strike Slip ◽  
Red River Fault ◽  
Strike Slip Movement ◽  
Geological Analysis

Late Quaternary activity and dextral strike-slip movement on the Karakax Fault Zone, northwest Tibet

2008 ◽  
Vol 453 (1-4) ◽  
pp. 44-62 ◽  
Author(s):  
Aiming Lin ◽  
Ken-ichi Kano ◽  
Jianming Guo ◽  
Tadashi Maruyama
Keyword(s):  
Fault Zone ◽  
Late Quaternary ◽  
Strike Slip ◽  
Dextral Strike Slip ◽  
Strike Slip Movement

Mesozoic strike-slip movement of the Dunhua–Mishan Fault Zone in NE China: A response to oceanic plate subduction

2018 ◽  
Vol 723 ◽  
pp. 201-222 ◽  
Author(s):  
Cheng Liu ◽  
Guang Zhu ◽  
Shuai Zhang ◽  
Chengchuan Gu ◽  
Yunjian Li ◽  
...  
Keyword(s):  
Fault Zone ◽  
Strike Slip ◽  
Oceanic Plate ◽  
Ne China ◽  
Plate Subduction ◽  
Strike Slip Movement

scholarly journals Kinematic partitioning in the Southern Andes (39° S–46° S) inferred from lineament analysis and reassessment of exhumation rates

2021 ◽  
Author(s):  
Paul Leon Göllner ◽  
Jan Oliver Eisermann ◽  
Catalina Balbis ◽  
Ivan A. Petrinovic ◽  
Ulrich Riller
Keyword(s):  
Fault Zone ◽  
Vertical Displacement ◽  
Strike Slip ◽  
Structural Studies ◽  
Southern Andes ◽  
Plate Convergence ◽  
Exhumation Rates ◽  
Lineament Analysis ◽  
Dextral Strike Slip ◽  
Data Call

AbstractThe Southern Andes are often viewed as a classic example for kinematic partitioning of oblique plate convergence into components of continental margin-parallel strike-slip and transverse shortening. In this regard, the Liquiñe-Ofqui Fault Zone, one of Earth’s most prominent intra-arc deformation zones, is believed to be the most important crustal discontinuity in the Southern Andes taking up margin-parallel dextral strike-slip. Recent structural studies, however, are at odds with this simple concept of kinematic partitioning, due to the presence of margin-oblique and a number of other margin-parallel intra-arc deformation zones. However, knowledge on the extent of such zones in the Southern Andes is still limited. Here, we document traces of prominent structural discontinuities (lineaments) from the Southern Andes between 39° S and 46° S. In combination with compiled low-temperature thermochronology data and interpolation of respective exhumation rates, we revisit the issue of kinematic partitioning in the Southern Andes. Exhumation rates are maximal in the central parts of the orogen and discontinuity traces, trending predominantly N–S, WNW–ESE and NE–SW, are distributed across the entire width of the orogen. Notably, discontinuities coincide spatially with large gradients in Neogene exhumation rates and separate crustal domains characterized by uniform exhumation. Collectively, these relationships point to significant components of vertical displacement on these discontinuities, in addition to horizontal displacements known from published structural studies. Our results agree with previously documented Neogene shortening in the Southern Andes and indicate orogen-scale transpression with maximal vertical extrusion of rocks in the center of the transpression zone. The lineament and thermochronology data call into question the traditional view of kinematic partitioning in the Southern Andes, in which deformation is focused on the Liquiñe-Ofqui Fault Zone.

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