Log in
Language:

MERAL Myanmar Education Research and Learning Portal

  • Top
  • Universities
  • Ranking
To
lat lon distance
To

Field does not validate



Index Link

Index Tree

Please input email address.

WEKO

One fine body…

WEKO

One fine body…

Item

{"_buckets": {"deposit": "64bc0642-6ed2-45cd-8626-cd52b54ebaba"}, "_deposit": {"created_by": 232, "id": "12770", "owner": "232", "owners": [232], "owners_ext": {"displayname": "", "username": ""}, "pid": {"revision_id": 0, "type": "depid", "value": "12770"}, "status": "published"}, "_oai": {"id": "oai:meral.edu.mm:recid/00012770", "sets": ["1704332280616", "1704445069427"]}, "author_link": [], "item_1583103067471": {"attribute_name": "Title", "attribute_value_mlt": [{"subitem_1551255647225": "Petrographic and Geochemical Characteristics of Granitic Mylonite and its Tectonic Significance Exposed in the Kabani Area, Wundwin Township, Mandalay Region", "subitem_1551255648112": "en"}]}, "item_1583103085720": {"attribute_name": "Description", "attribute_value_mlt": [{"interim": "The study area, located in the Kabani region of Wundwin Township, lies within the northern segment of Myanmar’s Central Granitoid Belt, bounded by the Sagaing Fault to the west and the Nwalabo Fault Complex to the east. Detailed field and microscopic investigations reveal that the granitic rocks have undergone intense ductile deformation, resulting in well-developed mylonitic textures such as foliation, lineation, and grain size reduction. The geochemical data, including major, trace, and rare earth elements, indicate that the granitic mylonites belong mainly to the calc-alkaline series and are classified as S-type granitoids. Harker variation diagrams demonstrate a fractional crystallization trend, while trace element plots reveal significant enrichment in LILEs and negative anomalies in HFSEs, suggesting crustal influence and subduction-related signatures. Tectonic discrimination diagrams such as the Rb–(Y+Nb), Nb–Y, and R₁–R₂ plots suggest that the protoliths of these granitic mylonites formed in a syn- to post-collisional tectonic setting."}]}, "item_1583103108160": {"attribute_name": "Keywords", "attribute_value_mlt": [{"interim": "Central Granitoid Belt"}, {"interim": "Harker variation diagrams"}, {"interim": "mylonitic textures"}]}, "item_1583103120197": {"attribute_name": "Files", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_access", "date": [{"dateType": "Available", "dateValue": "2026-06-01"}], "displaytype": "preview", "download_preview_message": "", "file_order": 0, "filename": "Petrographic and Geochemical Characteristics of Granitic Mylonite and its Tectonic Significance Exposed in the Kabani Area, Wundwin Township, Mandalay Region.pdf", "filesize": [{"value": "1.5 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_0", "mimetype": "application/pdf", "size": 1500000.0, "url": {"url": "https://meral.edu.mm/record/12770/files/Petrographic and Geochemical Characteristics of Granitic Mylonite and its Tectonic Significance Exposed in the Kabani Area, Wundwin Township, Mandalay Region.pdf"}, "version_id": "35bd956f-0e18-476a-93b4-d303e7746824"}]}, "item_1583103131163": {"attribute_name": "Journal articles", "attribute_value_mlt": [{"subitem_journal_title": "Kyaukse University Research Journal", "subitem_pages": "352-364", "subitem_volume": "IV"}]}, "item_1583105942107": {"attribute_name": "Authors", "attribute_value_mlt": [{"subitem_authors": [{"subitem_authors_fullname": "Nay Win Aung"}, {"subitem_authors_fullname": "Thu Rein Soe"}, {"subitem_authors_fullname": "Wai Wai Thin"}]}]}, "item_1583108359239": {"attribute_name": "Upload type", "attribute_value_mlt": [{"interim": "Publication"}]}, "item_1583108428133": {"attribute_name": "Publication type", "attribute_value_mlt": [{"interim": "Journal article"}]}, "item_1583159729339": {"attribute_name": "Publication date", "attribute_value": "2025-12-01"}, "item_title": "Petrographic and Geochemical Characteristics of Granitic Mylonite and its Tectonic Significance Exposed in the Kabani Area, Wundwin Township, Mandalay Region", "item_type_id": "21", "owner": "232", "path": ["1704332280616", "1704445069427"], "permalink_uri": "https://meral.edu.mm/records/12770", "pubdate": {"attribute_name": "Deposit date", "attribute_value": "2026-06-01"}, "publish_date": "2026-06-01", "publish_status": "0", "recid": "12770", "relation": {}, "relation_version_is_last": true, "title": ["Petrographic and Geochemical Characteristics of Granitic Mylonite and its Tectonic Significance Exposed in the Kabani Area, Wundwin Township, Mandalay Region"], "weko_shared_id": -1}
  1. Kyaukse University
  1. Kyaukse University
  2. Geology Department

Petrographic and Geochemical Characteristics of Granitic Mylonite and its Tectonic Significance Exposed in the Kabani Area, Wundwin Township, Mandalay Region

https://meral.edu.mm/records/12770
https://meral.edu.mm/records/12770
7446060d-0980-433d-a7af-9ad8dd24faba
64bc0642-6ed2-45cd-8626-cd52b54ebaba
None
Preview
Name / File License Actions
Petrographic Petrographic and Geochemical Characteristics of Granitic Mylonite and its Tectonic Significance Exposed in the Kabani Area, Wundwin Township, Mandalay Region.pdf (1.5 MB)
license.icon
Publication type
Journal article
Upload type
Publication
Title
Title Petrographic and Geochemical Characteristics of Granitic Mylonite and its Tectonic Significance Exposed in the Kabani Area, Wundwin Township, Mandalay Region
Language en
Publication date 2025-12-01
Authors
Nay Win Aung
Thu Rein Soe
Wai Wai Thin
Description
The study area, located in the Kabani region of Wundwin Township, lies within the northern segment of Myanmar’s Central Granitoid Belt, bounded by the Sagaing Fault to the west and the Nwalabo Fault Complex to the east. Detailed field and microscopic investigations reveal that the granitic rocks have undergone intense ductile deformation, resulting in well-developed mylonitic textures such as foliation, lineation, and grain size reduction. The geochemical data, including major, trace, and rare earth elements, indicate that the granitic mylonites belong mainly to the calc-alkaline series and are classified as S-type granitoids. Harker variation diagrams demonstrate a fractional crystallization trend, while trace element plots reveal significant enrichment in LILEs and negative anomalies in HFSEs, suggesting crustal influence and subduction-related signatures. Tectonic discrimination diagrams such as the Rb–(Y+Nb), Nb–Y, and R₁–R₂ plots suggest that the protoliths of these granitic mylonites formed in a syn- to post-collisional tectonic setting.
Keywords
Central Granitoid Belt, Harker variation diagrams, mylonitic textures
Journal articles
Kyaukse University Research Journal
352-364
IV
Back
0
0
views
downloads
See details
Views Downloads

Versions

Ver.1 2026-06-01 06:30:34.140624
Show All versions

Share

Mendeley Twitter Facebook Print Addthis

Export

OAI-PMH
  • OAI-PMH DublinCore
Other Formats
  • JSON

Confirm


Back to MERAL


Back to MERAL