{"created":"2020-03-08T23:26:52.513725+00:00","id":2132,"links":{},"metadata":{"_buckets":{"deposit":"fb8f343b-85f9-4fb5-8596-fac23d126209"},"_deposit":{"id":"2132","owners":[],"pid":{"revision_id":0,"type":"recid","value":"2132"},"status":"published"},"_oai":{"id":"oai:meral.edu.mm:recid/2132","sets":["1582963390870:1582967711045"]},"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":"2132","item_1583103067471":{"attribute_name":"Title","attribute_value_mlt":[{"subitem_1551255647225":"Marine transgression and regression in Miocene sequences of northern Pegu (Bago) Yoma, Central Myanmar","subitem_1551255648112":"en"}]},"item_1583103085720":{"attribute_name":"Description","attribute_value_mlt":[{"interim":"Neogene strata of the northern part of the Pegu (Bago) Yoma Range, Cent ral Myanmar , con ta in a series of shallow marine\r clastic sediments with stratigraphic ages ranging from the Earl y to Late Miocene. The studied succession (around 750 m thick ) is\r composed of three major stratigraphic unit s deposit ed during a major regression and four major transgressive cycles in the Early\r to Late Miocene. The transgressive deposit s consist of elongate sand-bars and broad sand-sheets that pass headward into mixedflats\r of tidal environments. Marine floodin g in transgressive deposits is associated with coquina beds and allochthonous coralbearing\r sandy limestone bands. Major marine regressions are associated with lowstand progradation of thick estuary point-bars\r passing up into upper sand-flat sand bodies encased within the tidal flat sequences and lower shoreface deposits with local\r unconformities. The succession initially formed in a large scale incised-valley system, and was later interrupted by two major\r marine transgressions in the generally regressive or basinward-stepping stratigraphic sequences. Successive sandbo dies were\r formed during a sea-level low stand and early stage of the subsequent relative rise of sea level in a tide-d ominated estu ary system\r in the eastern part of the Central Myanmar Tertiary Basin during Early to Late Miocene times. © 1999 Elsevier Science Ltd .\r All rights reserved."}]},"item_1583103108160":{"attribute_name":"Keywords"},"item_1583103131163":{"attribute_name":"Journal articles","attribute_value_mlt":[{"subitem_journal_title":"Journal of Asian Earth Sciences","subitem_volume":"17"}]},"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":"Kyi Khin"},{"subitem_authors_fullname":"Myitta"}]}]},"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":"1999"},"item_1583159847033":{"attribute_name":"Identifier","attribute_value":"http://uyr.uy.edu.mm/handle/123456789/190"},"item_title":"Marine transgression and regression in Miocene sequences of northern Pegu (Bago) Yoma, Central Myanmar","item_type_id":"21","owner":"1","path":["1582967711045"],"publish_date":"2020-03-05","publish_status":"0","recid":"2132","relation_version_is_last":true,"title":["Marine transgression and regression in Miocene sequences of northern Pegu (Bago) Yoma, Central Myanmar"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2021-12-13T01:39:34.589774+00:00"}