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    <title>UTas ePrints - Jurassic to Miocene magmatism and metamorphism in the Mogok metamorphic belt and the India-Eurasia collision in Myanmar</title>
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    <meta content="Barley, M.E." name="eprints.creators_name" />
<meta content="Pickard, A.L." name="eprints.creators_name" />
<meta content="Zaw, K." name="eprints.creators_name" />
<meta content="Rak, P." name="eprints.creators_name" />
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<meta content="Jurassic to Miocene magmatism and metamorphism in the Mogok
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<meta content="SE Asia, Myanmar, granitoids, metamorphism, zircon
dating, geochronology, SHRIMP, Granite, Mogok" name="eprints.keywords" />
<meta content="Situated south of the eastern Himalayan syntaxis at
the western margin of the Shan-Thai terrane the highgrade
Mogok metamorphic belt (MMB) in Myanmar occupies a key position in the tectonic evolution of Southeast Asia. The first sensitive high-resolution ion microprobe U-Pb in zircon geochronology for the MMB shows that strongly deformed granitic orthogneisses near Mandalay contain Jurassic (~170 Ma) zircons that have partly recrystallized during ~43 Ma high-grade metamorphism. A hornblende syenite
from Mandalay Hill also contains Jurassic zircons with
evidence of Eocene metamorphic recrystallization
rimmed by thin zones of 30.9 plus or minus 0.7 Ma magmatic
zircon. The relative abundance of Jurassic zircons in
these rocks is consistent with suggestions that southern
Eurasia had an Andean-type margin at that time. Mid-
Cretaceous to earliest Eocene (120 to 50 Ma) I-type
granitoids in the MMB, Myeik Archipelago, and Western Myanmar confirm that prior to the collision of India, an up to 200 km wide magmatic belt extended along the Eurasian margin from Pakistan to Sumatra. 
Metamorphic overgrowths to zircons in the orthogneiss
near Mandalay date a period of Eocene (~43 Ma)
high-grade metamorphism possibly during crustal
thickening related to the initial collision between
India and Eurasia (at 65 to 55 Ma). This was
followed by emplacement of syntectonic hornblende
syenites and leucogranites between 35 and 23 Ma.
Similar syntectonic syenites and leucogranites intruded
the Ailao Shan-Red River shear belt in southern China
and Vietnam during the Eocene-Oligocene to Miocene,
and the Wang Chao and Three Pagodas faults in
northern Thailand (that most likely link with the MMB)
were also active at this time. The complex history of
Eocene to early Miocene metamorphism, deformation,
and magmatism in the MMB provides evidence that it
may have played a key role in the network of
deformation zones that accommodated strain during
the northwards movement of India and resulting
extrusion or rotation of Indochina." name="eprints.abstract" />
<meta content="2003-05" name="eprints.date" />
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<meta content="Tectonics" name="eprints.publication" />
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<meta content="Bender, F., Geology of Burma, 1st ed., 293 pp., Gebruder
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Sagaing fault or the northward migration of the
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26, 915-918, 1999.
Brook, M., and N. J. Snelling, K/Ar and Rb/Sr age
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Dewey, J. F., S. Cande, and W. C. I. Pitman, Tectonic
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Multiple growth and recrystallization during polyphase
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in Applications of Microanalytical Techniques to Understanding Mineralization Processes, edited by M. A. McKibben, W. C. Shanks III, and W. I. Ridley, Rev. Econ. Geol., 7, 1-35, 1998. 
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in magmatic titanite and their consequence for the
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Zhang, L.-S., and U. Scharer, Age and origin of magmatism
along the Cenozoic Red River shear belt, China, Contrib. Mineral. Petrol., 134, 67-85, 1999." name="eprints.referencetext" />
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<meta content="Situated south of the eastern Himalayan syntaxis at
the western margin of the Shan-Thai terrane the highgrade
Mogok metamorphic belt (MMB) in Myanmar occupies a key position in the tectonic evolution of Southeast Asia. The first sensitive high-resolution ion microprobe U-Pb in zircon geochronology for the MMB shows that strongly deformed granitic orthogneisses near Mandalay contain Jurassic (~170 Ma) zircons that have partly recrystallized during ~43 Ma high-grade metamorphism. A hornblende syenite
from Mandalay Hill also contains Jurassic zircons with
evidence of Eocene metamorphic recrystallization
rimmed by thin zones of 30.9 plus or minus 0.7 Ma magmatic
zircon. The relative abundance of Jurassic zircons in
these rocks is consistent with suggestions that southern
Eurasia had an Andean-type margin at that time. Mid-
Cretaceous to earliest Eocene (120 to 50 Ma) I-type
granitoids in the MMB, Myeik Archipelago, and Western Myanmar confirm that prior to the collision of India, an up to 200 km wide magmatic belt extended along the Eurasian margin from Pakistan to Sumatra. 
Metamorphic overgrowths to zircons in the orthogneiss
near Mandalay date a period of Eocene (~43 Ma)
high-grade metamorphism possibly during crustal
thickening related to the initial collision between
India and Eurasia (at 65 to 55 Ma). This was
followed by emplacement of syntectonic hornblende
syenites and leucogranites between 35 and 23 Ma.
Similar syntectonic syenites and leucogranites intruded
the Ailao Shan-Red River shear belt in southern China
and Vietnam during the Eocene-Oligocene to Miocene,
and the Wang Chao and Three Pagodas faults in
northern Thailand (that most likely link with the MMB)
were also active at this time. The complex history of
Eocene to early Miocene metamorphism, deformation,
and magmatism in the MMB provides evidence that it
may have played a key role in the network of
deformation zones that accommodated strain during
the northwards movement of India and resulting
extrusion or rotation of Indochina." name="DC.description" />
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    <h1 class="ep_tm_pagetitle">Jurassic to Miocene magmatism and metamorphism in the Mogok metamorphic belt and the India-Eurasia collision in Myanmar</h1>
    <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Barley, M.E.</span> and <span class="person_name">Pickard, A.L.</span> and <span class="person_name">Zaw, K.</span> and <span class="person_name">Rak, P.</span> and <span class="person_name">Doyle, M.G.</span> (2003) <xhtml:em>Jurassic to Miocene magmatism and metamorphism in the Mogok metamorphic belt and the India-Eurasia collision in Myanmar.</xhtml:em> Tectonics, 22 (3). pp. 4-1. ISSN 0278-7407</p><p style="margin-bottom: 1em" class="not_ep_block"></p><table style="margin-bottom: 1em" class="not_ep_block"><tr><td valign="top" style="text-align:center"><a href="http://eprints.utas.edu.au/1879/1/Barley%2C_Pickard%2C_Zaw_et_al_TECTONICS_2003.pdf"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" border="0" class="ep_doc_icon" /></a></td><td valign="top"><a href="http://eprints.utas.edu.au/1879/1/Barley%2C_Pickard%2C_Zaw_et_al_TECTONICS_2003.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />770Kb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input value="2362" name="docid" accept-charset="utf-8" type="hidden" /><div class=""><input value="Request a copy" name="_action_null" class="ep_form_action_button" onclick="return EPJS_button_pushed( '_action_null' )" type="submit" /> </div></form></td></tr></table><p style="margin-bottom: 1em" class="not_ep_block">Official URL: <a href="http://dx.doi.org/10.1029/2002TC001398">http://dx.doi.org/10.1029/2002TC001398</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">Situated south of the eastern Himalayan syntaxis at&#13;
the western margin of the Shan-Thai terrane the highgrade&#13;
Mogok metamorphic belt (MMB) in Myanmar occupies a key position in the tectonic evolution of Southeast Asia. The first sensitive high-resolution ion microprobe U-Pb in zircon geochronology for the MMB shows that strongly deformed granitic orthogneisses near Mandalay contain Jurassic (~170 Ma) zircons that have partly recrystallized during ~43 Ma high-grade metamorphism. A hornblende syenite&#13;
from Mandalay Hill also contains Jurassic zircons with&#13;
evidence of Eocene metamorphic recrystallization&#13;
rimmed by thin zones of 30.9 plus or minus 0.7 Ma magmatic&#13;
zircon. The relative abundance of Jurassic zircons in&#13;
these rocks is consistent with suggestions that southern&#13;
Eurasia had an Andean-type margin at that time. Mid-&#13;
Cretaceous to earliest Eocene (120 to 50 Ma) I-type&#13;
granitoids in the MMB, Myeik Archipelago, and Western Myanmar confirm that prior to the collision of India, an up to 200 km wide magmatic belt extended along the Eurasian margin from Pakistan to Sumatra. &#13;
Metamorphic overgrowths to zircons in the orthogneiss&#13;
near Mandalay date a period of Eocene (~43 Ma)&#13;
high-grade metamorphism possibly during crustal&#13;
thickening related to the initial collision between&#13;
India and Eurasia (at 65 to 55 Ma). This was&#13;
followed by emplacement of syntectonic hornblende&#13;
syenites and leucogranites between 35 and 23 Ma.&#13;
Similar syntectonic syenites and leucogranites intruded&#13;
the Ailao Shan-Red River shear belt in southern China&#13;
and Vietnam during the Eocene-Oligocene to Miocene,&#13;
and the Wang Chao and Three Pagodas faults in&#13;
northern Thailand (that most likely link with the MMB)&#13;
were also active at this time. The complex history of&#13;
Eocene to early Miocene metamorphism, deformation,&#13;
and magmatism in the MMB provides evidence that it&#13;
may have played a key role in the network of&#13;
deformation zones that accommodated strain during&#13;
the northwards movement of India and resulting&#13;
extrusion or rotation of Indochina.</p></div><table style="margin-bottom: 1em" border="0" cellpadding="3" class="not_ep_block"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Article</td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">SE Asia, Myanmar, granitoids, metamorphism, zircon&#13;
dating, geochronology, SHRIMP, Granite, Mogok</td></tr><tr><th valign="top" class="ep_row">Subjects:</th><td valign="top" class="ep_row"><a href="http://eprints.utas.edu.au/view/subjects/260103.html">260000 Earth Sciences &gt; 260100 Geology &gt; 260103 Vulcanology</a><br /><a href="http://eprints.utas.edu.au/view/subjects/260100.html">260000 Earth Sciences &gt; 260100 Geology</a></td></tr><tr><th valign="top" class="ep_row">Collections:</th><td valign="top" class="ep_row">UNSPECIFIED</td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">1879</td></tr><tr><th valign="top" class="ep_row">Deposited By:</th><td valign="top" class="ep_row"><span class="ep_name_citation"><span class="person_name">Mrs Katrina Keep</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">07 Sep 2007</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">30 Jan 2008 15:26</td></tr><tr><th valign="top" class="ep_row">ePrint Statistics:</th><td valign="top" class="ep_row"><a target="ePrintStats" href="/es/index.php?action=show_detail_eprint;id=1879;">View statistics for this ePrint</a></td></tr></table><p align="right">Repository Staff Only: <a href="http://eprints.utas.edu.au/cgi/users/home?screen=EPrint::View&amp;eprintid=1879">item control page</a></p>
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