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": "4c5515ec-b56c-45de-bb40-f729d7858c9e"}, "_deposit": {"id": "2559", "owners": [], "pid": {"revision_id": 0, "type": "recid", "value": "2559"}, "status": "published"}, "_oai": {"id": "oai:meral.edu.mm:recid/2559", "sets": ["user-uy"]}, "communities": ["ccm", "ccp", "kyauksetu", "ltc", "maas", "miit", "mlmu", "mmu", "mtlu", "mtu", "mub", "mude", "mufl", "pathein", "scu", "suoe", "tcu", "tgu", "tuh", "tum", "ucsm", "ucsmtla", "ucsmub", "ucspathein", "ucstaungoo", "ucsy", "udmm", "udmy", "uit", "um", "um1", "um2", "umkn", "umm", "uphy", "urj", "uvs", "uy", "yau", "ydbu", "ytu", "yude", "yueco", "yufl", "yuoe"], "control_number": "2559", "item_1583103067471": {"attribute_name": "Title", "attribute_value_mlt": [{"subitem_1551255647225": "The Study of Folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division", "subitem_1551255648112": "en"}]}, "item_1583103085720": {"attribute_name": "Description", "attribute_value_mlt": [{"interim": "The Pinle-in area is mainly composed of metasedimentary rocks with some igneous intrusions. It is situated between Sagaing Fault and Shan-Scarp Fault in central Myanmar. The present study has carried out the systematic measurements of the plunge directions, plunge angles, thickness and distance of the limbs of minor folds in the calc-silicate rocks of Pinle-in area, Madaya and Singu Township, Mandalay Division. Similar plunge directions of folds are grouped as the zones. These zones are matched to speculate the possible explanation for where the hidden major fold is situated. The type of folds may be more or less anticline preferably overturned natures in the area. The axis of overturned anticline, likely to be double plunging, may be located along the Thabyaw Range with the direction of NNW-SSE and the Yetkanzin Range may also be assumed as the southern continuation of the Thabyaw Range."}]}, "item_1583103108160": {"attribute_name": "Keywords", "attribute_value_mlt": [{"interim": "Minor folds"}]}, "item_1583103120197": {"attribute_name": "Files", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_access", "date": [{"dateType": "Available", "dateValue": "2020-05-05"}], "displaytype": "preview", "download_preview_message": "", "file_order": 0, "filename": "The Study of folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division.pdf", "filesize": [{"value": "4769 Kb"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 4769000.0, "url": {"url": "https://meral.edu.mm/record/2559/files/The Study of folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division.pdf"}, "version_id": "f24c9429-b6ee-4a65-ad7b-89cdffbbdd3c"}]}, "item_1583103131163": {"attribute_name": "Journal articles", "attribute_value_mlt": [{"subitem_issue": "2", "subitem_journal_title": "Universities Research Journal (URJ)"}]}, "item_1583103147082": {"attribute_name": "Conference papaers", "attribute_value_mlt": [{}]}, "item_1583103211336": {"attribute_name": "Books/reports/chapters", "attribute_value_mlt": [{}]}, "item_1583103233624": {"attribute_name": "Thesis/dissertations", "attribute_value_mlt": [{"subitem_supervisor(s)": []}]}, "item_1583105942107": {"attribute_name": "Authors", "attribute_value_mlt": [{"subitem_authors": [{"subitem_authors_fullname": "Saw Ngwe Khaing"}]}]}, "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": "2008"}, "item_1583159847033": {"attribute_name": "Identifier", "attribute_value": "https://uyr.uy.edu.mm/handle/123456789/571"}, "item_title": "The Study of Folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division", "item_type_id": "21", "owner": "1", "path": ["1582967711045"], "permalink_uri": "http://hdl.handle.net/20.500.12678/0000002559", "pubdate": {"attribute_name": "Deposited date", "attribute_value": "2020-03-05"}, "publish_date": "2020-03-05", "publish_status": "0", "recid": "2559", "relation": {}, "relation_version_is_last": true, "title": ["The Study of Folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division"], "weko_shared_id": -1}
  1. University of Yangon
  2. Department of Geology

The Study of Folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division

http://hdl.handle.net/20.500.12678/0000002559
http://hdl.handle.net/20.500.12678/0000002559
826d78e6-1112-4447-a6d1-44c3bd18c9cd
4c5515ec-b56c-45de-bb40-f729d7858c9e
None
Preview
Name / File License Actions
The The Study of folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division.pdf (4769 Kb)
Publication type
Journal article
Upload type
Publication
Title
Title The Study of Folding in Calc-silicate Rocks of Pinle-in Area, Mandalay Division
Language en
Publication date 2008
Authors
Saw Ngwe Khaing
Description
The Pinle-in area is mainly composed of metasedimentary rocks with some igneous intrusions. It is situated between Sagaing Fault and Shan-Scarp Fault in central Myanmar. The present study has carried out the systematic measurements of the plunge directions, plunge angles, thickness and distance of the limbs of minor folds in the calc-silicate rocks of Pinle-in area, Madaya and Singu Township, Mandalay Division. Similar plunge directions of folds are grouped as the zones. These zones are matched to speculate the possible explanation for where the hidden major fold is situated. The type of folds may be more or less anticline preferably overturned natures in the area. The axis of overturned anticline, likely to be double plunging, may be located along the Thabyaw Range with the direction of NNW-SSE and the Yetkanzin Range may also be assumed as the southern continuation of the Thabyaw Range.
Keywords
Minor folds
Identifier https://uyr.uy.edu.mm/handle/123456789/571
Journal articles
2
Universities Research Journal (URJ)
Conference papaers
Books/reports/chapters
Thesis/dissertations
Back
0
0
views
downloads
See details
Views Downloads

Versions

Ver.1 2020-03-08 23:42:19.075327
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