Relevant bibliographies by topics / Khao Kwang Fold Thrust Belt

Academic literature on the topic 'Khao Kwang Fold Thrust Belt'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Khao Kwang Fold Thrust Belt"

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Morley, C. K., and S. Jitmahantakul. "Secondary detachments within carbonates of the Saraburi Group, Triassic Khao Khwang fold and Thrust Belt, Thailand." Journal of Structural Geology 140 (November 2020): 104162. http://dx.doi.org/10.1016/j.jsg.2020.104162.

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2

Hansberry, Rowan Lawrence, Rosalind King, Alan S. Collins, and Christopher K. Morley. "Complex structure of an upper-level shale detachment zone: Khao Khwang fold and thrust belt, Central Thailand." Journal of Structural Geology 67 (October 2014): 140–53. http://dx.doi.org/10.1016/j.jsg.2014.07.016.

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Arboit, Francesco, Alan S. Collins, Rosalind King, Christopher K. Morley, and Rowan Hansberry. "Structure of the Sibumasu–Indochina collision, central Thailand: A section through the Khao Khwang Fold and thrust belt." Journal of Asian Earth Sciences 95 (December 2014): 182–91. http://dx.doi.org/10.1016/j.jseaes.2014.06.016.

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4

Hansberry, Rowan L., Alan S. Collins, Rosalind C. King, Christopher K. Morley, Andy P. Giże, John Warren, Stefan C. Löhr, and P. A. Hall. "Syn-deformation temperature and fossil fluid pathways along an exhumed detachment zone, khao khwang fold-thrust belt, Thailand." Tectonophysics 655 (August 2015): 73–87. http://dx.doi.org/10.1016/j.tecto.2015.05.012.

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5

Morley, Christopher Keith, Sukonmeth Jitmahantakul, Sopon Pongwapee, and Hathaichanok Vattanasak. "Multiphase deformation of an inverted Permian deepwater rift basin: The Nong Pong Formation, Khao Khwang Fold and Thrust Belt, Thailand." Journal of Asian Earth Sciences 224 (February 2022): 104979. http://dx.doi.org/10.1016/j.jseaes.2021.104979.

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6

Morley, C. K., S. Jitmahantakul, C. von Hagke, J. Warren, and F. Linares. "Development of an intra-carbonate detachment during thrusting: The variable influence of pressure solution on deformation style, Khao Khwang Fold and Thrust Belt, Thailand." Geosphere 17, no. 2 (January 21, 2021): 602–25. http://dx.doi.org/10.1130/ges02267.1.

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Abstract Classic detachment zones in fold and thrust belts are generally defined by a weak lithology (typically salt or shale), often accompanied by high over-pressures. This study describes an atypical detachment that occurs entirely within a relatively strong Permian carbonate lithology, deformed during the Triassic Indosinian orogeny in Thailand under late diagenetic-anchimetamorphic conditions. The key differences between stratigraphic members that led to development of a detachment zone are bedding spacing and clay content. The lower, older, unit is the Khao Yai Member (KYM), which is a dark-gray to black, well-bedded, clay-rich limestone. The upper unit, the Na Phra Lan Member (NPM), comprises more massive, medium- to light-gray, commonly recrystallized limestones and marble. The KYM displays much tighter to even isoclinal, shorter-wavelength folds than the NPM. Pressure solution played a dominant role throughout the structural development—first forming early diagenetic bedding; later tectonic pressure solution preferentially followed this bedding instead of forming axial planar cleavage. The detachment zone between the two members is transitional over tens of meters. Moving up-section, tight to isoclinal folds with steeply inclined axial surfaces are replaced by folds with low-angle axial planes, thrusts, and thrust wedging, bed-parallel shearing, and by pressure solution along bedding-parallel seams (that reduce fold amplitude). In outcrops 100–300 m long, reduction of line-length shortening on folds from >50% to <10% shortening upwards indicates that deformation in the NPM is being accommodated differently from the KYM, probably predominantly by shortening on longer wavelength and/or spacing folds and thrusts, given the low amount of strain observed within the NPM, which excludes widespread layer-parallel thickening.
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Morley, C. K., P. Ampaiwan, S. Thanudamrong, N. Kuenphan, and J. Warren. "Development of the Khao Khwang Fold and Thrust Belt: Implications for the geodynamic setting of Thailand and Cambodia during the Indosinian Orogeny." Journal of Asian Earth Sciences 62 (January 2013): 705–19. http://dx.doi.org/10.1016/j.jseaes.2012.11.021.

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8

Vattanasak, Hathaichanok, Chongpan Chonglakmani, Qinglai Feng, and Christopher K. Morley. "Chert geochemistry, depositional setting, stratigraphic and structural significance for the Permian Nong Pong Formation, Khao Khwang Fold and Thrust Belt, Saraburi, Thailand." Journal of Asian Earth Sciences 191 (April 2020): 104234. http://dx.doi.org/10.1016/j.jseaes.2020.104234.

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9

Arboit, Francesco, Khalid Amrouch, Christopher Morley, Alan S. Collins, and Rosalind King. "Palaeostress magnitudes in the Khao Khwang fold-thrust belt, new insights into the tectonic evolution of the Indosinian orogeny in central Thailand." Tectonophysics 710-711 (July 2017): 266–76. http://dx.doi.org/10.1016/j.tecto.2017.01.008.

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10

Arboit, Francesco, Alan S. Collins, Christopher K. Morley, Fred Jourdan, Rosalind King, John Foden, and Khalid Amrouch. "Geochronological and geochemical studies of mafic and intermediate dykes from the Khao Khwang Fold–Thrust Belt: Implications for petrogenesis and tectonic evolution." Gondwana Research 36 (August 2016): 124–41. http://dx.doi.org/10.1016/j.gr.2016.04.005.

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Dissertations / Theses on the topic "Khao Kwang Fold Thrust Belt"

1

Simpson, A. D. W. "The Meso-Cenozoic deformation history of Thailand and Myanmar; insights from calcite U-Pb and apatite fission track thermochronology." Thesis, 2018. https://hdl.handle.net/2440/133682.

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Abstract:
This item is only available electronically.
Given the absence of suitable dating methods, the timing of low-temperature crustal deformation is usually established by indirect methods (such as apatite fission track (AFT) thermochronology). Few studies have previously ventured into directly constraining the absolute timing of brittle deformation (such as authigenic illite dating). U-Pb dating of calcite in tectonic veins represents a new method to potentially directly date brittle deformation events (Roberts and Walker, 2016). By utilising this method in combination with apatite U-Pb and fission track thermochronology, this study sheds new light on the upper crustal deformation history of Thailand and Myanmar. U-Pb calcite ages demonstrate tectonic activity at ~216-209Ma in the Khao Kwang Fold and Thrust Belt associated with the Indosinian stage 2 collision between the Sibumasu Block and the Indochina Block. Brittle deformation along the Three Pagodas Fault Zone (TPFZ) was dated at ~45Ma and ~24Ma (and possibly as recently as ~1.3Ma). AFT thermochronology suggests exhumation in the Tin province of southern Myanmar at ~26Ma-18Ma. These dates are in agreement with previous regional AFT studies in Thailand and with calcite U-Pb dates for the TPFZ, suggesting fault reactivation in response to the India-Eurasia collision and rifting in the Andaman Sea. Calcite U-Pb ages were obtained with uncertainties as low as ~1%, which is an unprecedented precision for the timing of brittle deformation. This work further demonstrates that calcite elemental mapping, in combination with U-Pb dating, can be used to distinguish different calcite growth events. Particularly enrichments in Mn or depletions in LREE concentrations in calcite seem useful to distinguish different fluids and associated calcite (re)crystallisation events. Although further work is required to enhance our understanding of both Pb diffusion in calcite as well as geochemical tracers for calcite recrystallization, the combination of calcite U-Pb with apatite fission track thermochronology is a promising novel tool to enhance our understanding of the timing of brittle deformation.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2018
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