Administratively the study area is located in Maja Village which situated near the border of between Sumedang and Majalengka Regency, West Jawa – Indonesia. Geographically located at coordinates 108°11'28" - 108°13'42" Longitude and 6°51'28" - 6°55'30' Lattitude. In the study area the Formation Cinambo was widely distributed. Geological observation was conducted in Cirompoki River, Kadu River, and Cimaningtim River such as outcrops description and detail measuring section and rock sampling for granulometry as well as biostratigraphy analysis. The stratigraphy of Cinambo Formation is divided into Claystone-sandstone unit (facies D), Sandstone-mudstone units (facies C), Sandstone Unit (facies B) and Claystone units (facies E). This formation deposited in the mechanism of high density turbidite current. Plankton fossils showed that this formation was deposited in Middle Miocene to Early Pliocene (N11-N18) in upper bathyal environment. Integrated result of sediment profiles and granulometry showed that sedimentation of Cinambo Formation had characteristics which are: coarsening upward, etc. The vertical succession of Fm. Cinambo sandstone caused by current mechanisms of saltation, suspension, traction, that changed according to depositional environment. This formation was deposited in the outer part of submarine fan change until its middle part. Environmental change caused by influenced of eustacy in relative sea level drop.
| Published in | Earth Sciences (Volume 8, Issue 3) |
| DOI | 10.11648/j.earth.20190803.17 |
| Page(s) | 190-204 |
| Creative Commons |
This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
| Copyright |
Copyright © The Author(s), 2019. Published by Science Publishing Group |
Turbidite, Fm. Cinambo, Granulometry, Eustacy
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APA Style
Yan Rizal, Wahyu Dwijo Santoso, Sapta Djanuismawan, Alfend Rudyawan, Affan Arif Nurfarhan. (2019). Sedimentation Study of Sandstone Turbidite Sequence of Cinambo Formation in Maja Area, Majalengka, West Jawa – Indonesia. Earth Sciences, 8(3), 190-204. https://doi.org/10.11648/j.earth.20190803.17
ACS Style
Yan Rizal; Wahyu Dwijo Santoso; Sapta Djanuismawan; Alfend Rudyawan; Affan Arif Nurfarhan. Sedimentation Study of Sandstone Turbidite Sequence of Cinambo Formation in Maja Area, Majalengka, West Jawa – Indonesia. Earth Sci. 2019, 8(3), 190-204. doi: 10.11648/j.earth.20190803.17
AMA Style
Yan Rizal, Wahyu Dwijo Santoso, Sapta Djanuismawan, Alfend Rudyawan, Affan Arif Nurfarhan. Sedimentation Study of Sandstone Turbidite Sequence of Cinambo Formation in Maja Area, Majalengka, West Jawa – Indonesia. Earth Sci. 2019;8(3):190-204. doi: 10.11648/j.earth.20190803.17
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author = {Yan Rizal and Wahyu Dwijo Santoso and Sapta Djanuismawan and Alfend Rudyawan and Affan Arif Nurfarhan},
title = {Sedimentation Study of Sandstone Turbidite Sequence of Cinambo Formation in Maja Area, Majalengka, West Jawa – Indonesia},
journal = {Earth Sciences},
volume = {8},
number = {3},
pages = {190-204},
doi = {10.11648/j.earth.20190803.17},
url = {https://doi.org/10.11648/j.earth.20190803.17},
eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20190803.17},
abstract = {Administratively the study area is located in Maja Village which situated near the border of between Sumedang and Majalengka Regency, West Jawa – Indonesia. Geographically located at coordinates 108°11'28" - 108°13'42" Longitude and 6°51'28" - 6°55'30' Lattitude. In the study area the Formation Cinambo was widely distributed. Geological observation was conducted in Cirompoki River, Kadu River, and Cimaningtim River such as outcrops description and detail measuring section and rock sampling for granulometry as well as biostratigraphy analysis. The stratigraphy of Cinambo Formation is divided into Claystone-sandstone unit (facies D), Sandstone-mudstone units (facies C), Sandstone Unit (facies B) and Claystone units (facies E). This formation deposited in the mechanism of high density turbidite current. Plankton fossils showed that this formation was deposited in Middle Miocene to Early Pliocene (N11-N18) in upper bathyal environment. Integrated result of sediment profiles and granulometry showed that sedimentation of Cinambo Formation had characteristics which are: coarsening upward, etc. The vertical succession of Fm. Cinambo sandstone caused by current mechanisms of saltation, suspension, traction, that changed according to depositional environment. This formation was deposited in the outer part of submarine fan change until its middle part. Environmental change caused by influenced of eustacy in relative sea level drop.},
year = {2019}
}
TY - JOUR T1 - Sedimentation Study of Sandstone Turbidite Sequence of Cinambo Formation in Maja Area, Majalengka, West Jawa – Indonesia AU - Yan Rizal AU - Wahyu Dwijo Santoso AU - Sapta Djanuismawan AU - Alfend Rudyawan AU - Affan Arif Nurfarhan Y1 - 2019/07/10 PY - 2019 N1 - https://doi.org/10.11648/j.earth.20190803.17 DO - 10.11648/j.earth.20190803.17 T2 - Earth Sciences JF - Earth Sciences JO - Earth Sciences SP - 190 EP - 204 PB - Science Publishing Group SN - 2328-5982 UR - https://doi.org/10.11648/j.earth.20190803.17 AB - Administratively the study area is located in Maja Village which situated near the border of between Sumedang and Majalengka Regency, West Jawa – Indonesia. Geographically located at coordinates 108°11'28" - 108°13'42" Longitude and 6°51'28" - 6°55'30' Lattitude. In the study area the Formation Cinambo was widely distributed. Geological observation was conducted in Cirompoki River, Kadu River, and Cimaningtim River such as outcrops description and detail measuring section and rock sampling for granulometry as well as biostratigraphy analysis. The stratigraphy of Cinambo Formation is divided into Claystone-sandstone unit (facies D), Sandstone-mudstone units (facies C), Sandstone Unit (facies B) and Claystone units (facies E). This formation deposited in the mechanism of high density turbidite current. Plankton fossils showed that this formation was deposited in Middle Miocene to Early Pliocene (N11-N18) in upper bathyal environment. Integrated result of sediment profiles and granulometry showed that sedimentation of Cinambo Formation had characteristics which are: coarsening upward, etc. The vertical succession of Fm. Cinambo sandstone caused by current mechanisms of saltation, suspension, traction, that changed according to depositional environment. This formation was deposited in the outer part of submarine fan change until its middle part. Environmental change caused by influenced of eustacy in relative sea level drop. VL - 8 IS - 3 ER -
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