Log in
Language:

MERAL Myanmar Education Research and Learning Portal

  • MERAL
  • Universities
  • Ranking
AND
To


Index Link

Index Tree

WEKO

One fine body…

Item

{"_buckets": {"deposit": "72c4a1b1-eb7c-4e02-b50f-61ce5441ed2c"}, "_deposit": {"id": "547", "owners": [], "pid": {"revision_id": 0, "type": "recid", "value": "547"}, "status": "published"}, "_oai": {"id": "oai:meral.edu.mm:recid/547"}, "control_number": "547", "item_1583103067471": {"attribute_name": "Title", "attribute_value_mlt": [{"subitem_1551255647225": "Sedimentological log of the upper pegu group exposed in Natogyi-Taungthar Area, Mandalay Region", "subitem_1551255648112": "en"}]}, "item_1583103085720": {"attribute_name": "Description", "attribute_value_mlt": [{"interim": "The study area is situated about 6 miles southwest of the Natogyi Township, Mandalay Division. The field area lies between East Longitude 95\uf0b030\u0027 to 95\uf0b041\u0027and North Latitude 21\uf0b015\u0027 to 21\uf0b026\u0027 in one-inch topographic map 84 O/11. The stratigraphic succession of the study area in ascending order is: (1) Moza Formation (Middle Miocene), (2) Khabo Sandstone (Upper part of Middle Miocene) and (3) Irrawaddy Formation (Pontian to Pliocene). The detailed graphic logs were constructed in a tabulated form by plotting sedimentary features such as structures on bedding plane, structures within the layers, fossil content, etc. and these features were represented by means of symbols. The graphic log of Moza Formation consists of 51 layers and has a total thickness of about 3200 centimeters. It can be divided into four units. The graphic log of Khabo Sandstone contains 148 layers and attains nearly 4130 centimeters in thickness. It can be divided into five units. The frequency of vertical layer thickness variation of these two formations is quite different. It is clear that the beds of Khabo Sandstone are thicker than those of Maza Formation. According to the study of sedimentological log, Moza Formation was deposited under a fairly variable hydrodynamic regime of deltaic environment. On the other hand, the sediments which belong to the Khabo Sandstone were deposited under more turbulent flow conditions."}]}, "item_1583103108160": {"attribute_name": "Keywords", "attribute_value_mlt": [{"interim": "Sedimentological log"}]}, "item_1583103120197": {"attribute_name": "Files", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_access", "date": [{"dateType": "Available", "dateValue": "2020-05-05"}], "displaytype": "preview", "filename": "SEDIMENTOLOGICAL LOG OF THE UPPER PEGU GROUP.pdf", "filesize": [{"value": "2590 Kb"}], "format": "application/pdf", "licensetype": "license_free", "mimetype": "application/pdf"}]}, "item_1583103131163": {"attribute_name": "Journal articles", "attribute_value_mlt": [{"subitem_issue": "1", "subitem_journal_title": "Lashio University Research Journal", "subitem_volume": "4"}]}, "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": "Htay Win"}]}]}, "item_1583108359239": {"attribute_name": "Upload Type", "attribute_name_i18n": "Upload Type", "attribute_value": "Publication"}, "item_1583108428133": {"attribute_name": "Publication type", "attribute_name_i18n": "Publication type", "attribute_value": "Journal article"}, "item_1583159729339": {"attribute_name": "Publication date", "attribute_name_i18n": "Publication date", "attribute_value": "2012"}, "item_title": "Sedimentological log of the upper pegu group exposed in Natogyi-Taungthar Area, Mandalay Region", "item_type_id": "21", "owner": "1", "path": ["1582963788001/1582966668038"], "permalink_uri": "http://hdl.handle.net/20.500.12678/0000000547", "publish_date": "2020-03-05", "publish_status": "0", "recid": "547", "relation": {}, "relation_version_is_last": true, "title": ["Sedimentological log of the upper pegu group exposed in Natogyi-Taungthar Area, Mandalay Region"], "weko_creator_id": "1", "weko_shared_id": -1}
  1. Yadanabon University
  2. Department of Geology

Sedimentological log of the upper pegu group exposed in Natogyi-Taungthar Area, Mandalay Region

Permalink : http://hdl.handle.net/20.500.12678/0000000547
b2d83217-67e2-492d-95a4-f4ea07651818
72c4a1b1-eb7c-4e02-b50f-61ce5441ed2c
Preview
Name / File License Actions
SEDIMENTOLOGICAL SEDIMENTOLOGICAL LOG OF THE UPPER PEGU GROUP.pdf (2.6 MB)
sha256: 008fb220d52c66a47e705dc7985c5e9ea1782ac4e0cb9e5596f95cfaba0929c7
Publication type Journal article
Upload Type Publication
Title
Sedimentological log of the upper pegu group exposed in Natogyi-Taungthar Area, Mandalay Region
en
Publication date 2012
Authors
Htay Win
Description
The study area is situated about 6 miles southwest of the Natogyi Township, Mandalay Division. The field area lies between East Longitude 9530' to 9541'and North Latitude 2115' to 2126' in one-inch topographic map 84 O/11. The stratigraphic succession of the study area in ascending order is: (1) Moza Formation (Middle Miocene), (2) Khabo Sandstone (Upper part of Middle Miocene) and (3) Irrawaddy Formation (Pontian to Pliocene). The detailed graphic logs were constructed in a tabulated form by plotting sedimentary features such as structures on bedding plane, structures within the layers, fossil content, etc. and these features were represented by means of symbols. The graphic log of Moza Formation consists of 51 layers and has a total thickness of about 3200 centimeters. It can be divided into four units. The graphic log of Khabo Sandstone contains 148 layers and attains nearly 4130 centimeters in thickness. It can be divided into five units. The frequency of vertical layer thickness variation of these two formations is quite different. It is clear that the beds of Khabo Sandstone are thicker than those of Maza Formation. According to the study of sedimentological log, Moza Formation was deposited under a fairly variable hydrodynamic regime of deltaic environment. On the other hand, the sediments which belong to the Khabo Sandstone were deposited under more turbulent flow conditions.
Keywords
Sedimentological log
Files 2590 Kb
Available
2020-05-05
application/pdf
preview
application/pdf
open_access
SEDIMENTOLOGICAL LOG OF THE UPPER PEGU GROUP.pdf

Journal articles
1
Lashio University Research Journal
4
Conference papaers
Books/reports/chapters
Thesis/dissertations
Back
0
0
views
downloads
See details
Views Downloads

Versions

Ver.1 2020-03-08 08:07:46.485063
Show All versions

Share

Mendeley CiteULike Twitter Facebook Print Addthis

Export

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

Confirm


Back to MERAL


Back to MERAL