PHILLIPSITE MINERAL IN DEEP SEA SEDIMENT FROM SINGLE CORE IN ROO RISE, INDIAN OCEAN
During the MD III - IMAGES IV Expedition, one of the cores that has length around 30.30 m below sea floor (bsf) was obtained using gigantic piston corer from the depth of 3,884 m below sea level (bsl). This core (MD982156) is located in Roo Rise, Indian Ocean, south of East Jawa, outer part of Jawa...
Main Authors: | , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Puslitbang tekMIRA
2017
|
Subjects: | |
Online Access: | https://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/612 https://doi.org/10.30556/imj.Vol10.No3.2007.612 |
id |
ftpuslitbangbatu:oai:ojs.jurnal.tekmira.esdm.go.id:article/612 |
---|---|
record_format |
openpolar |
spelling |
ftpuslitbangbatu:oai:ojs.jurnal.tekmira.esdm.go.id:article/612 2023-05-15T18:00:35+02:00 PHILLIPSITE MINERAL IN DEEP SEA SEDIMENT FROM SINGLE CORE IN ROO RISE, INDIAN OCEAN ADISAPUTRA, MIMIN K. HARTONO, HARTONO 2017-11-22 application/pdf https://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/612 https://doi.org/10.30556/imj.Vol10.No3.2007.612 eng eng Puslitbang tekMIRA https://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/612/474 https://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/612 doi:10.30556/imj.Vol10.No3.2007.612 ##submission.copyrightStatement## http://creativecommons.org/licenses/by-nc/4.0 CC-BY-NC Indonesian Mining Journal; Vol 10, No 3 (2007): INDONESIAN MINING JOURNAL Vol. 10 No. 3 October 2007; 39 - 43 2527-8797 0854-9931 Phillipsite deep sea Roo Rise south of East Java Indian Ocean info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2017 ftpuslitbangbatu https://doi.org/10.30556/imj.Vol10.No3.2007.612 2021-04-24T18:19:44Z During the MD III - IMAGES IV Expedition, one of the cores that has length around 30.30 m below sea floor (bsf) was obtained using gigantic piston corer from the depth of 3,884 m below sea level (bsl). This core (MD982156) is located in Roo Rise, Indian Ocean, south of East Jawa, outer part of Jawa Trench. The sediment consists of abundance planktonic foraminifera in the upper part while in the lower part, there is no planktonic one. The latter is mostly composed of phillipsite-rich sediment (± 40%) that is possibly derived from tephra. The base of the core between the depths of 30 – 30.30 m bsf is composed of clay sediment, consisting of minerals derived from zeolite group (phillipsite), gibbsite, and other cryptocrystalline masses. Phillipsite was deposited as an authigenic deep sea sediment, whereas gibbsite is usually deposited within bodies of water. Besides, there are also nanno- plankton accumulated in the crystal of phillipsite. This part has an age of Late Miocene or older. This fact is supported by the overlain layer containing planktonic foraminifera species Sphaeroidinellopsis seminulina of Late Miocene age (N17). The thickness and the lateral continuity of this layer are still unknown. Article in Journal/Newspaper Planktonic foraminifera Jurnal Puslitbang tekMira (Teknologi Mineral dan Batubara) Indian |
institution |
Open Polar |
collection |
Jurnal Puslitbang tekMira (Teknologi Mineral dan Batubara) |
op_collection_id |
ftpuslitbangbatu |
language |
English |
topic |
Phillipsite deep sea Roo Rise south of East Java Indian Ocean |
spellingShingle |
Phillipsite deep sea Roo Rise south of East Java Indian Ocean ADISAPUTRA, MIMIN K. HARTONO, HARTONO PHILLIPSITE MINERAL IN DEEP SEA SEDIMENT FROM SINGLE CORE IN ROO RISE, INDIAN OCEAN |
topic_facet |
Phillipsite deep sea Roo Rise south of East Java Indian Ocean |
description |
During the MD III - IMAGES IV Expedition, one of the cores that has length around 30.30 m below sea floor (bsf) was obtained using gigantic piston corer from the depth of 3,884 m below sea level (bsl). This core (MD982156) is located in Roo Rise, Indian Ocean, south of East Jawa, outer part of Jawa Trench. The sediment consists of abundance planktonic foraminifera in the upper part while in the lower part, there is no planktonic one. The latter is mostly composed of phillipsite-rich sediment (± 40%) that is possibly derived from tephra. The base of the core between the depths of 30 – 30.30 m bsf is composed of clay sediment, consisting of minerals derived from zeolite group (phillipsite), gibbsite, and other cryptocrystalline masses. Phillipsite was deposited as an authigenic deep sea sediment, whereas gibbsite is usually deposited within bodies of water. Besides, there are also nanno- plankton accumulated in the crystal of phillipsite. This part has an age of Late Miocene or older. This fact is supported by the overlain layer containing planktonic foraminifera species Sphaeroidinellopsis seminulina of Late Miocene age (N17). The thickness and the lateral continuity of this layer are still unknown. |
format |
Article in Journal/Newspaper |
author |
ADISAPUTRA, MIMIN K. HARTONO, HARTONO |
author_facet |
ADISAPUTRA, MIMIN K. HARTONO, HARTONO |
author_sort |
ADISAPUTRA, MIMIN K. |
title |
PHILLIPSITE MINERAL IN DEEP SEA SEDIMENT FROM SINGLE CORE IN ROO RISE, INDIAN OCEAN |
title_short |
PHILLIPSITE MINERAL IN DEEP SEA SEDIMENT FROM SINGLE CORE IN ROO RISE, INDIAN OCEAN |
title_full |
PHILLIPSITE MINERAL IN DEEP SEA SEDIMENT FROM SINGLE CORE IN ROO RISE, INDIAN OCEAN |
title_fullStr |
PHILLIPSITE MINERAL IN DEEP SEA SEDIMENT FROM SINGLE CORE IN ROO RISE, INDIAN OCEAN |
title_full_unstemmed |
PHILLIPSITE MINERAL IN DEEP SEA SEDIMENT FROM SINGLE CORE IN ROO RISE, INDIAN OCEAN |
title_sort |
phillipsite mineral in deep sea sediment from single core in roo rise, indian ocean |
publisher |
Puslitbang tekMIRA |
publishDate |
2017 |
url |
https://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/612 https://doi.org/10.30556/imj.Vol10.No3.2007.612 |
geographic |
Indian |
geographic_facet |
Indian |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Indonesian Mining Journal; Vol 10, No 3 (2007): INDONESIAN MINING JOURNAL Vol. 10 No. 3 October 2007; 39 - 43 2527-8797 0854-9931 |
op_relation |
https://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/612/474 https://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/612 doi:10.30556/imj.Vol10.No3.2007.612 |
op_rights |
##submission.copyrightStatement## http://creativecommons.org/licenses/by-nc/4.0 |
op_rightsnorm |
CC-BY-NC |
op_doi |
https://doi.org/10.30556/imj.Vol10.No3.2007.612 |
_version_ |
1766169756504686592 |