MICROFACIES OF LOWER JONGGRANGAN FORMATION AT BRAJAN SECTION, BANJARARUM, KULON PROGO, INDONESIA
|
|
- Lawrence Clark
- 6 years ago
- Views:
Transcription
1 MICROFACIES OF LOWER JONGGRANGAN FORMATION AT BRAJAN SECTION, BANJARARUM, KULON PROGO, INDONESIA Setyo PAMBUDI1,2*, Vijaya ISNANIAWARDHANI1, WINANTRIS1, Adjat SUDRADJAT1 1 2 Faculty of Geological Engineering, Padjadjaran University, Bandung Department of Geological Engineering, Sekolah Tinggi Teknologi Nasional (STTNAS) Yogyakarta, *Corresponding author: pambudisetyo@yahoo.com ABSTRACT The Jonggrangan Formation is one of the carbonate rock units of West Progo Hill exposed in Brajan, Banjararum, West Progo. The aim of this study is determining the environment and depositional mechanism of the lower Jonggrangan Formation at Brajan, Banjararum, West Progo. Petrographic analysis was used to find out the standard of microfacies while paleontological analysis have been done to determine the age and sedimentary environment. Based on stratigraphic measurement section at Brajan area, the lower Jonggrangan Formation is generally dominated by limestones, sandy limestone and intercalation of calcareous sandstone. Results of petrographic analysis show that the type of rocks are floatstone, packstone, sandy lime packstone, sandy lime wackestone and calcareous lithic arenite. The results of standard microfacies analysis show that the rocks have been deposited on the foreslope (SMF5 / FZ4), deep shelf margin (SMF5 / FZ3) and open sea shelf (SMF9 / FZ2) environments. Paleontological data indicates that sedimentary rocks deposited during the Early Miocene to lower Middle Miocene (N5 - N9) in inner middle neritic environment. Keywords: Microfacies, Jonggrangan Formation, limestone, Brajan. INTRODUCTION The Kulon Progo Hills have been extensively researched by several geologists from Indonesia and abroad (Table 1). The experts who have conducted the researchs are Marks (1957), Bemmelen (1949), Darwin Kadar (1976, 1981), Suyanto & Roskamil (1975), Rahardjo, et al (1977), Harsono & Purnamaningsih (1981), Suroso et al (1986), Harsono & Riyanto (1987) and Soeria - Atmadja, et al (1991). Jonggrangan Formation is composed of reef limestone, always in high altitude, overlain unconformably on Old Andesit Formation. The study of microfacies limestone aims to determine the environment and the depositional mechanism of the lower Jonggrangan Formation in Brajan area. The research was conducted in Brajan, Banjararum, Kalibawang, Kulon Progo District, Yogyakarta (Figure 1). 268
2 LITERATURE REVIEW The Kulon Progo Hills are an elongated dome-shaped ridges in the northeast-southwest direction (Bemmelen, 1949). Stratigraphy from previous researchers can be concluded that the regional stratigraphy of Kulon Progo Hills from old to young namely: Nanggulan Formation, Old Andesite Formation, Jonggrangan Formation, Sentolo Formation and Alluvium Depositions (Table 1). The Nanggulan Formation (Middle Late Eocene) is composed by sandstones, upwardly transformed into alternating sandstones and lignite-containing clay. The top of the Nanggulan Formation consists of the marl and carbonate sandstones called as the Seputih Member. The Old Andesite Formation (Oligocene) is composed of volcanic breccia, lava, lapilli breccia, lapilli tuff and sandstone, deposited unconformably on Nanggulan Formation. The Jonggrangan Formation (Early Miocene - Late Miocene) is composed by a tuffaceous marl, a carbonate sandstone with lignite inserts that upward turn into a layered limestone and a coral boulder that forms a reef. This formation is unconformable on Old Andesite Formation. The Sentolo Formation (Early Miocene - Pliocene) is composed of limestone, sandstone, fine tuffaceous marl with abundant foraminifera fossils content. The Sentolo formation is unconformable on Old Andesite Formation. While for Alluvium Deposits, Rahardjo (1977) said the Yogyakarta Formation, composed by Merapi volcano rocks and alluvial sediment of the river that is still ongoing until now. This unit is overlay unconformably on the older rock units. Figure 1. Location of research area. 269
3 Table 1. Stratigraphy of Kulon Progo area according to some previous researchers. METHODS Petrographic testing of several rock samples was used to sharpen the analysis and interpretation of sedimentology aspects, particularly aspects of the microfacies of limestones. The classification of limestone types is based on the classification Dunham (1962), whereas non-carbonate rocks classification use Pettijohn s (1975). Paleontological analysis is used to determine the age and depositional environment of the rocks. Analysis of microfacies by Flugel (1982) and facial belt according to Wilson (1975). RESULT AND DISCUSSION Stratigraphic measurements in the Brajan, Banjararum, Kulonprogo regions are regionally included in the Old Andesite Formation and Jonggrangan Formation (Rahardjo et al, 1977). The Old Andesite Formation is composed of andesite breccia, overlain unconformably by Jonggrangan Formation, composed of limestones, sandy limestone and calcareous sandstones (Table 2). The results of the planktonic foraminifera analysis of Jonggrangan Formation in the Brajan region showed Early Miocene - early Middle Miocene (N5 - N9) age, ie the discovery of Globigerina binaiensis Koch, Globigerinoides trilobus (Reuss), Globigerinoides sacculiferus (Brady), Globigeinopides diminutus Bolli, Praeorbulina glomerosa Blow, Orbulina universa D'Orbigny. The results of the benthonic analysis showed that Jonggrangan Formation are deposited in the Inner Neritic Middle Neritic, ie the finding of Amphistegina lessonii D'Orbigny, Operculina complanata Defrance, Buccella parkerae Andrean, Anomalina colligera (Chapman & Parr), Nodosaria sp. Petrographic observations refer to Dunham (1962), Embry & Klovan (1971), the division of 270
4 microfasies according to Flugel (1982), which is the development of facial belts according to Wilson (1975). The observations from the bottom up in the example of SP-BRJ 01 showed floatstone type rock, in the example of SP-BRJ 02 showed rocks of the packstone type. Both rocks are deposited in the foreslope denoted by SMF5 / FZ4. In the example of SP-BRJ 04, SP-BRJ 06, SP-BRJ 07 rocks of sandy lime packestone, deposited in a deep shelf margin denoted by SMF5 / FZ3. At the top of the samples are SP-BRJ 10 and SP-BRJ 11 rocks of the sandy lime wackestone, deposited on open sea shelf denoted by SMF9 / FZ2. The intercalation of non-carbonate rock is calcareous lithic arenite as found in the example of SPBRJ 03, SP-BRJ 05, SP-BRJ 08 and SP-BRJ 09. The first tectonic phase that occurred in Kulon Progo Hill at Oligocene - Early Miocene was followed by active volcanic activity that produced three volcanous were Gajah, Ijo and Menoreh which have source of eruption in high altitude (Bemmelen, 1949). In the research area it is represented by andesite breccia of Old Andesite Formation. In the second tectonic phase of the Early Miocene there was subsidence of Kulon Progo area, causing the height area become the sea and deposited the reef limestone of Jonggrangan Formation. Thus, the stratigraphy in the Kulon Progo Hills shows that the Jonggrangan Formation is unconformably overlain on ride above the Old Andesite Formation. In the research area, sedimentation of limestone of Jonggrangan Formation much influenced by volcanism activities to form a sandy that is sandy lime packstone - sandy lime wackestone. CONCLUSION The Jonggrangan Formation in the Brajan, Banjararum, Kulon Progo region is composed of limestone, sandy limestone, and calcareous sandstone of Early - Middle (N5 - N9), deposited at the inner middle neritic, overlain unconformably on Old Andesite Formation, beginning the deposition of floatstone and packstone in foreslope environment (SMF5 / FZ4), then sedimented of sandy lime packstone in deep shelf margin (SMF5 / FZ3) environment. At the top is deposited sandy lime wackestone in open sea shelf (SMF9 / FZ2). The non-carbonate rock intercalation is calcareous lithic arenite. The deposition of Jonggrangan Formation was still influenced by volcanic activity. 271
5 Table 2. Jonggrangan Formation stratigraphic column in Brajan area. 272
6 ACKNOWLEDGEMENT The authors would like to thank the Chairman of STTNAS who has financed the research and Joint Conference in Japan. REFERENCES Bemmelen, R.W. van The Geology of Indonesia. Vol.1A. Netherland: Government Printing Office, Martinus Nijhoff, The Hague. 732 p. Dunham, R.J Classification of Carbonate Rocks According to Depositional Texture. Dalam Ham, W.W. Classification of Carbonate Rocks. AAPG Mem. p Harsono, P. dan Purnamaningsih, S Stratigraphy and Planktonic Foraminifera of the Eocene Oligocene Nanggulan Formation, Central Java. Geol. Res. Dev. Centre Paleontology Series. Bandung. No. 1, pp Hartono, H.G. dan Pambudi, S Gunung Api Purba Mujil, Kulonprogo, Yogyakarta: Suatu Bukti dan Pemikiran. Prosiding ReTII ke 10. Yogyakarta : STTNAS. Kadar, D Planktonic Foraminifera Biostratigraphy of the Sentolo Formation, Central Java, Indonesia. Proc. the first International Conggres on Pacific Neogene Stratigraphy. Bandung. Pringgoprawiro, H. & Riyanto, B Formasi Andesit Tua Suatu Revisi. Proc. PIT IAGI XVI. Bandung: IAGI. Martodjojo, S. dan Pulunggono, A Perubahan Tektonik Paleogen-Neogen Merupakan Peristiwa Tektonik Terpenting di Jawa. Prosiding Geologi dan Geotektonik Pulau Jawa sejak Akhir Mesozoik hingga Kuarter. Yogyakarta: Jurusan T. Geologi Fak. Teknik UGM. hal Pambudi, S., Sutarman, dan Budiadi, Ev Pola Sedimentasi Formasi Jonggrangan Sentolo di Gunung Kucir Gunung Dlanggung Barat, Kec. Samigaluh dan Kec. Kalibawang, Kab. Kulonprogo. Jurnal Teknologi Nasional, Vol. II No. 1. Yogyakarta :STTNAS. Pettijohn, F.L Sedimentary Rocks. 3rd. Ed. New York: Harper & Row Publ. 628 p. Postuma, J.A Manual of Planktonic Foraminifera. Amsterdam: Elsevier Publ. Co. 420 p. Rahardjo, W., Sukandarrumidi, & Rosidi, H.M.S Peta Geologi Lembar Yogyakarta. Skala 1 : Bandung: Direktorat Geologi. Soeria-Atmadja, R., Maory, R.C., Bellon, Pringgoprawiro, H., Polve, M., & Priadi, B The Tertiary Magmatic Belt in Java. Proc. of Symposium in the Dynamic of Subduction and Its Products. Yogyakarta: Puslitbang Geoteknologi-LIPI. p Sujanto, F. X., and Sumantri, Y. R Preliminary Study of Tertiery Depositional Patterns of Java. Proc. of IPA, 6th and Conv. Jakarta: IPA. pp Suroso, P., Achmad, R., & Sutanto Usulan Penyesuaian Tata Nama Litostratigrafi Kulon Progo, DIY. Proc. PIT XV IAGI. Yogyakarta: IAGI. h Suyanto, F.X. dan Roskamil The Geology and Hydrocarbon Aspect of the South Central Java. Proc. of Indonesion Association of Geologists. Bandung: IAGI. 273
The analysis of volcanic activity influences at the lower and middle part of Sentolo Formation, Kulon Progo using petrographic method
The analysis of volcanic activity influences at the lower and middle part of Sentolo Formation, Kulon Progo using petrographic method Tri Winarno 1,*, Jenian Marin 1, Ilham Hani Pratama 1, and Anis Kurniasih
More informationHYDROISOTOPE OF GROUNDWATER IN WESTERNPART OF WEST PROGO DOME
KURVATEK Vol. 2. No. 1, April 2017, pp.14-19 ISSN: 2477-7870 14 HYDROISOTOPE OF GROUNDWATER IN WESTERNPART OF WEST PROGO DOME T. Listyani R.A. Jurusan Teknik Geologi, Sekolah Tinggi Teknologi Nasional
More informationTectonic Influence on Changes in Neogene Sediment Supply, Western Part of North Serayu Basin. B. S. Astuti 1, and H. D. Kusuma 1
Tectonic Influence on Changes in Neogene Sediment Supply, Western Part of North Serayu Basin B. S. Astuti 1, and H. D. Kusuma 1 ¹Department of Geology Sekolah Tinggi Teknologi Nasional Yogyakarta email:
More informationMICRO TECTONIC AT NORTH SERAYU BASIN, CENTRAL JAVA: CASE STUDY AT TYPE LOCALITY OF RAMBATAN FORMATION
MICRO TECTONIC AT NORTH SERAYU BASIN, CENTRAL JAVA: CASE STUDY AT TYPE LOCALITY OF RAMBATAN FORMATION Bernadeta Subandini ASTUTI*1,2, Vijaya ISNANIAWARDHANI 2, ABDURROKHIM 2, and Adjat SUDRADJAT2 1Department
More informationQUANTITATIVE CHARACTERIZATION OF CARBONATE PORE SYSTEMS ON JONGGRANGAN FORMATION USING DIGITAL IMAGE ANALYSIS (DIA)
QUANTITATIVE CHARACTERIZATION OF CARBONATE PORE SYSTEMS ON JONGGRANGAN FORMATION USING DIGITAL IMAGE ANALYSIS (DIA) Ari Wibowo 1*, Nana Higiana Hasanah 2 1 Department of Geological Engineering, UPN Veteran
More informationLINEAMENT CONTROL ON SPRING CHARACTERISTICS AT CENTRAL WEST PROGO HILLS, INDONESIA
Geotec., Const. Mat. & Env., DOI: https://doi.org/10.21660/2018.46.70127 ISSN: 2186-2982 (Print), 2186-2990 (Online), Japan LINEAMENT CONTROL ON SPRING CHARACTERISTICS AT CENTRAL WEST PROGO HILLS, INDONESIA
More informationSeismotectonic Analysis to Interpretation Fault Zone and Subduction Zone in West Java. How much effective?
Seismotectonic Analysis to Interpretation Fault Zone and Subduction Zone in West Java. How much effective? Nouval Wibowo, N. 1 Rosyadi, H. 1 1 PetroClan, University of Pembangunan Nasional Veteran, Yogyakarta,
More informationISOTOPIC CHEMICAL CHARACTERISTICS OF GROUNDWATER IN BANJARARUM AREA, WEST PROGO
KURVATEK Vol. 2. No. 2, November 2017, pp.25-33 ISSN: 2477-7870 25 ISOTOPIC CHEMICAL CHARACTERISTICS OF GROUNDWATER IN BANJARARUM AREA, WEST PROGO Sri Ning Peni & T. Listyani R.A. Geological Engineering
More informationADVENTINO1, Djohan Rizal PRASETYA1, M. Faris RAFFI1, Harry PRAMUDITO2, Sofyan RACHMAN2
THE IMPLICATION OF ANCIENT VOLCANO FOR DEVELOPMENT OF ENVIRONMENT FACTOR AND SOCIETY LIFE, CASE STUDY: MOUNT GADUNG AND SURROUNDING AREA, CENTRAL JAVA PROVINCE, INDONESIA ADVENTINO1, Djohan Rizal PRASETYA1,
More informationHYDROCHEMISTRY OF GROUNDWATER IN GEYER, GROBOGAN PROVINCE, CENTRAL JAVA
KURVATEK Vol. 1, No. 2, November 2016, pp. 13 19 ISSN: 2477-7870 13 HYDROCHEMISTRY OF GROUNDWATER IN GEYER, GROBOGAN PROVINCE, CENTRAL JAVA T. Listyani R.A. Geological Department, Sekolah Tinggi Teknologi
More informationMeutia Farida1, Pratiwi1, Ratna Husain1
Paleotemperature of Middle Eocene Tonasa Limestone based on Foraminifera at Palakka Area South Sulawesi Meutia Farida1, Pratiwi1, Ratna Husain1 1 Department of Geology, Hasanuddin University, Makassar,
More informationGeologic Structural Identification from 3D Stratigraphic Modeling of Geologic Map
Geologic Structural Identification from 3D Stratigraphic Modeling of Geologic Map Alva Kurniawan 1 Abstract Three dimensions stratigraphic model can be created from geologic stratigraphic data of geologic
More informationSismanto Geophysics Laboratory, Department of Physics, Faculty of Mathematics and Natural Science University of Gadjah Mada, Indonesia
International Journal of Civil Engineering and Technology (IJCIET) Volume 9, Issue 6, June 2018, pp. 1141 1150, Article ID: IJCIET_09_06_129 Available online at http://www.iaeme.com/ijciet/issues.asp?jtype=ijciet&vtype=9&itype=6
More informationChapter 3. Geology & Tectonics
Chapter 3 Geology & Tectonics 3.1 Geology The general geological features of Indonesia are shown in Figure 3.1. The basement formation is metamorphic and it is intruded with plutonic formations. They are
More informationPROCEEDINGS, INDONESIAN PETROLEUM ASSOCIATION Forty-First Annual Convention & Exhibition, May 2017
IPA17-369-SG PROCEEDINGS, INDONESIAN PETROLEUM ASSOCIATION Forty-First Annual Convention & Exhibition, May 2017 FACIES ANALYSIS OF LATE NEOGENE DEPOSIT: MARINE TO CONTINENTAL ENVIRONMENT OF THE MERAPI
More informationSearch and Discovery Article #11007 (2017)** Posted November 13, 2017
Click to view slide presentation (4.5 MB). Controlling Factor in Pliocene Carbonate Reservoir Quality as Key to Evaluate Play Chances: Case Study from Mundu Carbonate from South Madura Strait - East Java
More informationIDENTIFICATION SLIP SURFACE USING RESISTIVITY AND VLF-R MODE IN GOA KISKENDO YOGYAKARTA INDONESIA
Geotec., Const. Mat. & Env., DOI: https://doi.org/10.21660/2019.53.43734 ISSN: 2186-2982 (Print), 2186-2990 (Online), Japan IDENTIFICATION SLIP SURFACE USING RESISTIVITY AND VLF-R MODE IN GOA KISKENDO
More information1 st International Conference
New Perspective On High Grade Metamorphic Regional In Bayah Complex, Banten Province 1 st International Conference Geoscience for Energy, Mineral Resources, and Environment applieds 2014 Aton Patonah 1,
More informationDistribution of Ostracoda from Measured Section Data at Cimerang River, Sukabumi, Jawa Barat
Distribution of Ostracoda from Measured Section Data at Cimerang River, Sukabumi, Jawa Barat Mohamad Solihin 1, Prasma Feby Rahmadhani 1, Renanda Sevirajati 1, Hendy Taufik 1, Lili Fauzielly 1 1 Faculty
More informationJOURNAL OF GEOLOGICAL SCIENCES AND APPLIED GEOLOGY VOL.2, NO.1 APRIL 2017
Tephrostratigraphy Study Using Petrographic Method in Leles Sub-basin, Bogor, West Java Dea Carrisa D., M. Nashir., Yoga Andriana S, Nisa Nurul Ilmi, Edy Sunardi. Geological Engineering Faculty, Universitas
More informationSlope Stability Zonation Map of the Citanduy River Catchment Area, West Java, Indonesia. Irvan Sophian* and Dicky Muslim* Abstract
Slope Stability Zonation Map of the Citanduy River Catchment Area, West Java, Indonesia Irvan Sophian* and Dicky Muslim* Abstract In Indonesia, West Java Province is well known for the most frequent landslide
More informationSUBSURFACE MODELING OF YOGYAKARTA BASIN USING INVERSION METHOD OF GRAVITY DATA
SUBSURFACE MODELING OF YOGYAKARTA BASIN USING INVERSION METHOD OF GRAVITY DATA *Irham Nurwidyanto M. 1, Kirbani S.B. 2, Sismanto 2 and Waluyo 2 1 Department of Physics, Diponegoro University Semarang,
More informationControlling Groudwater System by Pattern Fracture Approach in Subsurface Volcanic Deposit: Mt.Salak- Mt.Pangranggo, West Java, Indonesia
IOP Conference Series: Earth and Environmental Science OPEN ACCESS Controlling Groudwater System by Pattern Fracture Approach in Subsurface Volcanic Deposit: Mt.Salak- Mt.Pangranggo, West Java, Indonesia
More informationNannoplankton Population as Indicator of Sea Level Change in Gunung Panti Area, North East Java Basin
Proceeding of International Conference of Transdisciplinary Research on Environmental Problem in Southeastern Asia 2014 Nannoplankton Population as Indicator of Sea Level Change in Gunung Panti Area, North
More informationStratigraphy Seismic and sedimentation Development of Middle Baong Sand, Aru Field, North Sumatera Basin
Journal of Geoscience, Engineering, Environment, and Technology Vol 01 No 01 2017 E-ISSN : 2541-5794 P-ISSN : 2503-216X Stratigraphy Seismic and sedimentation Development of Middle Baong Sand, Aru Field,
More informationMORPHOTECTONIC ASPECT TO DELINEATE MULTIHAZARD AREAS BASED ON SPATIAL ANALYSIS
MORPHOTECTONIC ASPECT TO DELINEATE MULTIHAZARD AREAS BASED ON SPATIAL ANALYSIS Cipta ENDYANA1,2,*, Febri HIRNAWAN1, Dicky MUSLIM1, Satoshi YAMAOKA3 1 Faculty of Geological Engineering, Universitas Padjadjaran,
More informationLiquefaction Potential Post-Earthquake in Yogyakarta
The 17 th Southeast Asian Geotechnical Conference Taipei, Taiwan, May 10~13, 2010 Liquefaction Potential Post-Earthquake in Yogyakarta AGUS SETYO MUNTOHAR 1 and S.P.R. WARDANI 2 1 Department of Civil Engineering,
More informationThe Subsurface Soil Effects Study Using the Short and Long Predominant Periods From H/V Spectrum In Yogyakarta City
Paper ID 90 The Subsurface Soil Effects Study Using the Short and Long Predominant Periods From H/V Spectrum In Yogyakarta City Z.L. Kyaw 1,2*, S. Pramumijoyo 2, S. Husein 2, T.F. Fathani 3, J. Kiyono
More informationPROCEEDINGS PIT IAGI YOGYAKARTA 2012 The 41 st IAGI Annual Convention and Exhibition
EG-25 COMPARING QUALITATIVE AND QUANTITATIVE METHOD TO DETERMINE EARTHQUAKE SUSCEPTIBILITY LEVEL AT KULON PROGO, YOGYAKARTA by: Deasy Rimanda Cahyaningtyas (1), Prof. Dr. Kirbani Sri Brotopuspito (2) Salahuddin
More informationDepositional History and Petroleum Potential of Ombilin Basin, West Sumatra - Indonesia, Based on Surface Geological Data*
Depositional History and Petroleum Potential of Ombilin Basin, West Sumatra - Indonesia, Based on Surface Geological Data* Yahdi Zaim 1, Litto Habrianta 2, Chalid I. Abdullah 1, Aswan 1, Yan Rizal 1, Nurcahyo
More informationSimon F. Mitchell. Field Trip 1: Geology of the White Limestone between Middlesex and Riverhead, Parish of St. Ann, Jamaica
Field Trip 1: Geology of the White Limestone between Middlesex and Riverhead, Parish of St. Ann, Jamaica Simon F. Mitchell Department of Geography and Geology, the University of the West Indies, Mona,
More informationIndonesian Journal on Geoscience, Vol. 2 No. 3 December 2015: netic process is the key to a good determination of carbonate reservoirs (Walker
Indonesian Journal on Geoscience Vol. 2 No. 3 December 2015: 157-166 INDONESIAN JOURNAL ON GEOSCIENCE Geological Agency Ministry of Energy and Mineral Resources Facies and Diagenetic Level of the Upper
More informationPetrology and Alteration of Lari Mountain in Arinem Area, West Java, Indonesia
Petrology and Alteration of Lari Mountain in Arinem Area, West Java, Indonesia Fatoni Adyahya 1 *, Euis T. Yuningsih 1, Ildrem Syafrie 1, H. Matsueda 2, A. Hardiyono 1 1 Faculty of Geology, University
More informationLIMESTONE POTENTIAL IN CIKATOMAS REGION BASED ON GEOLOGICAL MAPPING AND IT S ROLE TOWARDS DEVELOPMENT OF SOUTHERN PART OF WEST JAVA, INDONESIA
LIMESTONE POTENTIAL IN CIKATOMAS REGION BASED ON GEOLOGICAL MAPPING AND IT S ROLE TOWARDS DEVELOPMENT OF SOUTHERN PART OF WEST JAVA, INDONESIA Presented at the FIG Working Week 2016, May 2-6, 2016 in Christchurch,
More informationBiostratigraphic and Lithostratigraphic Correlation of Sedimentary Strata in the Atlantic Coastal Plain
Biostratigraphic and Lithostratigraphic Correlation of Sedimentary Strata in the Atlantic Coastal Plain Introduction to the Atlantic Coastal Plain (Please read this page prior to doing the lab) The Atlantic
More informationHirofumi Yamasaki, Morihisa Suzuki, Koki Harada, Takaaki Suga and Takehiro Hayashi
Hirofumi Yamasaki, Morihisa Suzuki, Koki Harada, Takaaki Suga and Takehiro Hayashi In the recent geologic years, age of the formations has been reexamined (e.g. Matsubara, 2009). Previously, most of the
More informationReservoir Description using Hydraulic Flow Unit and Petrophysical Rock Type of PMT Carbonate Early Miocene of Baturaja Formation, South Sumatra Basin*
Reservoir Description using Hydraulic Flow Unit and Petrophysical Rock Type of PMT Carbonate Early Miocene of Baturaja Formation, South Sumatra Basin* Jaka Radiansyah 1, Teddy E. Putra 1, Rienno Ismail
More informationThe Truth about Paroxysmal Merapi Volcano s Eruption from Geomorphology of Southwestern Merapi s Fluviovolcanic Plain
Proceeding International Geomorphologist Seminar Yogyakarta, Indonesia, 2008 The Truth about Paroxysmal Merapi Volcano s Eruption from Geomorphology of Southwestern Merapi s Fluviovolcanic Plain Alva Kurniawan
More informationTurbidite Fasies of Lower Penosogan Formation in Karanggayam Area, Kebumen, Indonesia
Modern Applied Science; Vol. 12, No. 6; 2018 ISSN 1913-1844 E-ISSN 1913-1852 Published by Canadian Center of Science and Education Turbidite Fasies of Lower Penosogan Formation in Karanggayam Area, Kebumen,
More informationDAFTAR PUSTAKA. Anonim, 1993, Topaz Field Report, PT. Caltex Pacific Indonesia
DAFTAR PUSTAKA Anonim, 1994, The Central Sumatra Basin: Central Sumatra Basin Geologic Setting, Indonesian Petroleum Association Seismic Atlas of Indonesian Oil and Gas Fields Sumatra Anonim, 1993, Topaz
More informationCHARACTERISTIC AND THE OCCURRENCE OF COAL DEPOSITS IN NEOGENE MANDAR FORMATION OF WEST SULAWESI PROVINCE
CHARACTERISTIC AND THE OCCURRENCE OF COAL DEPOSITS IN NEOGENE MANDAR FORMATION OF WEST SULAWESI PROVINCE Sufriadin1*, Asri Jaya H.S2 & A.M. Imran2 1Mining Engineering Study Program, Hasanuddin University,
More informationSedimentary Cycle Best Practice: Potential Eo-Oligocene Sediments in Western Indonesia*
Sedimentary Cycle Best Practice: Potential Eo-Oligocene Sediments in Western Indonesia* Mellinda Arisandy 1 and I Wayan Darma 1 Search and Discovery Article #11008 (2017)** Posted November 6, 2017 *Adapted
More informationGravity Data Analysis and Modelling for Basin Sedimen of Eastern Java Blocks
Journal of Physics: Conference Series PAPER OPEN ACCESS Gravity Data Analysis and Modelling for Basin Sedimen of Eastern Java Blocks To cite this article: Luthfia Khoirunnia 2016 J. Phys.: Conf. Ser. 776
More informationThe Occurrences of Base Metal Mineralization in Cikadu-Cisungsang Area, Banten Province, Indonesia*)
The Occurrences of Base Metal Mineralization in Cikadu-Cisungsang Area, Banten Province, Indonesia*) Rosana, M.F., Haryanto, A.D., Yuniardi, Y., Yuningsih, E.T. Department of Geology, Padjadjaran University
More informationPaleoecology and Paleoclimate of Tanjung Formation Deposition, Based on Palynological Data From Siung Malopot, Central Borneo
IOP Conference Series: Earth and Environmental Science OPEN ACCESS Paleoecology and Paleoclimate of Tanjung Formation Deposition, Based on Palynological Data From Siung Malopot, Central Borneo To cite
More informationBALOCHISTAN FOLDBELT BASIN
INTRODUCTION BALOCHISTAN FOLDBELT BASIN The Kharan-3 block is located in the Kharan Trough of Balochistan Basin. GEOLOGICAL SETTING The Balochistan Province is an Upper Cretaceous to Recent structurally
More informationStratigraphic Plays in Active Margin Basin: Fluvio-Deltaic Reservoir Distribution in Ciputat Half Graben, Northwest Java Basin*
Stratigraphic Plays in Active Margin Basin: Fluvio-Deltaic Reservoir Distribution in Ciputat Half Graben, Northwest Java Basin* Ary Wahyu Wibowo 1, Astri Pujianto 1, Wisnu Hindadari 1, Arief Wahidin Soedjono
More informationBuried Temple Ruin Parts Discovering on the Peak of Gunungsari Hill by Using Electrical Resistivity Tomography Survey within Wenner Schlumberger Array
Buried Temple Ruin Parts Discovering on the Peak of Gunungsari Hill by Using Electrical Resistivity Tomography Survey within Wenner Schlumberger Array Alva Kurniawan 1 Abstract According to Shearer and
More informationTectonics Activity and Volcanism Influence to the Garut and Leles Basins Configuration and the Implication on Environmental Geology
Tectonics Activity and Volcanism Influence to the Garut and Leles Basins Configuration and the Implication on Environmental Geology Iyan Haryanto 1, Emi Sukiyah 2, N. Nurul Ilmi 3, Y. A. Sendjaja 4, E.
More informationSedimentary facies and sequence stratigraphy of the Asmari Formation at Tange Arabi,Zagros Basin, Iran
Sedimentary facies and sequence stratigraphy of the Asmari Formation at Tange Arabi,Zagros Basin, Iran Atefe Abbasi, Geology student of Shiraz Payam-noor University Abstract The Oligocene Miocene ASMARI
More informationTHE APPLICATION OF VOLCANIC FACIES CONCEPT IN THE DESCRIPTION OF THE OLD ANDESITE FORMATION. By : Adjat Sudradjat 1 & Gendoet Hartono 2.
THE APPLICATION OF VOLCANIC FACIES CONCEPT IN THE DESCRIPTION OF THE OLD ANDESITE FORMATION By : Adjat Sudradjat 1 & Gendoet Hartono 2 Abstract Old Andesite Formation was ascribed to the ancient succession
More informationApplication of Aquifer Vulnerability Index (AVI) method to assess groundwater vulnerability to contamination in Semarang urban area
Application of Aquifer Vulnerability Index (AVI) method to assess groundwater vulnerability to contamination in Semarang urban area Thomas Triadi Putranto 1*, Narulita Santi 1, Dian Agus Widiarso 1, and
More informationJOURNAL OF GEOLOGICAL SCIENCES AND APPLIED GEOLOGY VOL.2, NO.1 APRIL Jalan Raya Bandung-Sumedang Km 21, Jatinangor
THE SALT POTENTIALS IN INDONESIA Emi Sukiyah 1, Vijaya Isnaniawardhani 1, Adjat Sudradjat 1 and Faisal Muhamadsyah 1 1 Faculty of Engineering Geology, Padjadjaran University Jalan Raya Bandung-Sumedang
More informationStratigraphy, Facies and Sedimentary Environments of Pliocene Deposits in the North of Tabriz, Iran
J. Basic. Appl. Sci. Res., 2(11)11878-11883, 2012 2012, TextRoad Publication ISSN 2090-4304 Journal of Basic and Applied Scientific Research www.textroad.com Stratigraphy, Facies and Sedimentary Environments
More informationCorals from the member C of Mobarak Formation in the Vali-Abad section (Central Alborz North part of Iran)
Corals from the member C of Mobarak Formation in the Vali-Abad section (Central Alborz North part of Iran) 1 Fatemeh Rezvan.nia, 2 Khaveh Khaksar, 3 Mohamad.R.Kebriaee.zade, 4 Rahim Shabanian 1 Geology
More informationFACIES MODELING OF KAIS FORMATION LIMESTONE: A CASE STUDY OF KAFOR FIELD, WEST PAPUA, INDONESIA
6 Special Issue on Science, Engineering & Environment, ISSN: 2186-2990, Japan DOI: https://doi.org/10.21660/2017.40.69647 FACIES MODELING OF KAIS FORMATION LIMESTONE: A CASE STUDY OF KAFOR FIELD, WEST
More informationPseudo 3d Gravity Modeling to Determine Intrusion Contact of Parang Area, Karangsambung, Central java, Jndonesia
2012 International Conference on Geological and Environmental Sciences IPCBEE vol.3 6(2012) (2012)ICSIT Press, Singapoore Pseudo 3d Gravity Modeling to Determine Intrusion Contact of Parang rea, Karangsambung,
More informationCharacteristic of the deep-water channels in the Lower Miocene Pulau Balang Formation in Samarinda
Characteristic of the deep-water channels in the Lower Miocene Pulau Balang Formation in Samarinda Abdurrokhim*, Djadjang J Setiadi, Faisal Helmi, Adi Hardiyono, and Yoga A Sendjaja Faculty of Geology,
More informationInvestigation of possible tsunami events on the eastern coast of Taiwan: case studies of Lu-Ye, Changping, and Tulan
Investigation of possible tsunami events on the eastern coast of Taiwan: case studies of Lu-Ye, Changping, and Tulan Speaker : FX. Anjar Tri Laksono Adviser : Louis Loung-Yie Tsai Date : October 19, 2017
More informationEruptive History of Tangkuban Perahu Volcano, West Java, Indonesia: A Preliminary Report
Reports and Subsidiary Research in 2001 Eruptive History of Tangkuban Perahu Volcano, West Java, Indonesia: A Preliminary Report Mochamad Nugraha KARTADINATA*, Mitsuru OKUNO**, Toshio NAKAMURA*** and Tetsuo
More informationStudy on Improvement of Dumping Site Stability in Weak Geological Condition by Using Compacted Layer
Open Journal of Geology, 2015, 5, 144-155 Published Online March 2015 in SciRes. http://www.scirp.org/journal/ojg http://dx.doi.org/10.4236/ojg.2015.53014 Study on Improvement of Dumping Site Stability
More information*Twin H. W. Kristyanto Geology Study Program, FMIPA UI, Universitas Indonesia, Indonesia *Author for Correspondence:
GAMMA RAY EMISSION IN NEOTECTONIC ZONE OF BANDUNG AREA *Twin H. W. Kristyanto Geology Study Program, FMIPA UI, Universitas Indonesia, Indonesia *Author for Correspondence: twin.hosea@sci.ui.ac.id ABSTRACT
More informationOn the Geomorphology and Tectonic Position of Ciletuh-Jampang Area, West Java, Indonesia
Universal Journal of Geoscience 6(2): 47-54, 2018 DOI: 10.13189/ujg.2018.060203 http://www.hrpub.org On the Geomorphology and Tectonic Position of Ciletuh-Jampang Area, West Java, Indonesia Iyan Haryanto,
More informationMonday 23 May 2016 Morning
Oxford Cambridge and RSA Monday 23 May 2016 Morning AS GCE GEOLOGY F792/01 Rocks Processes and Products *6008024131* Candidates answer on the Question Paper. OCR supplied materials: None Other materials
More informationPROCEEDINGS, INDONESIAN PETROLEUM ASSOCIATION Twenty Seventh Annual Convention & Exhibition, October 1999
IPA99-G-046 PROCEEDINGS, INDONESIAN PETROLEUM ASSOCIATION Twenty Seventh Annual Convention & Exhibition, October 1999 THE CENOZOIC EVOLUTION OF THE LARIANG AND KARAMA BASINS, SULAWESI Stephen J. Calvert*
More informationON THE GEOMORPHOLOGY AND TECTONIC POSITION OF CILETUH-JAMPANG AREA WEST JAVA, INDONESIA 1
ON THE GEOMORPHOLOGY AND TECTONIC POSITION OF CILETUH-JAMPANG AREA WEST JAVA, INDONESIA 1 Nana Sulaksana 2, Iyan Haryantho 2, Emi Sukiyah 2 and Adjat Sudradjat 2 1 Presented at the Conference organized
More informationAnalysis of Structural Geology based on Sattelite Image and Geological Mapping on Binuang Area, Tapin Region, South Kalimantan
Analysis of Structural Geology based on Sattelite Image and Geological Mapping on Binuang Area, Tapin Region, South Kalimantan Tiggi Choanji 1, Rahmat Indrajati 2 ABSTRACT Study area lies on Binuang, Binuang
More informationGEOMORPHOLOGY APPROACH IN LANDSLIDE VULNERABILITY, TANJUNG PALAS TENGAH, EAST KALIMANTAN, INDONESIA
GEOMORPHOLOGY APPROACH IN LANDSLIDE VULNERABILITY, TANJUNG PALAS TENGAH, EAST KALIMANTAN, INDONESIA *Twin H. W. Kristyanto Geology Study Program, FMIPA UI, Universitas Indonesia *Author for Correspondence:
More informationPROCEEDINGS, INDONESIAN PETROLEUM ASSOCIATION Thirty-Ninth Annual Convention and Exhibition, May 2015
IPA15-SG-089 PROCEEDINGS, INDONESIAN PETROLEUM ASSOCIATION Thirty-Ninth Annual Convention and Exhibition, May 2015 STRUCTURAL INTERPRETATION OF TECTONICALLY ASSOCIATED NORMAL AND REVERSE FAULTS OF BUKIT
More informationGeochemical Study of Ampallas Geothermal Area, Mamuju District, West Sulawesi Province
IOP Conference Series: Earth and Environmental Science PAPER OPEN ACCESS Geochemical Study of Ampallas Geothermal Area, Mamuju District, West Sulawesi Province To cite this article: F Fauziyyah et al 2016
More informationTHE FORAMINIFERAL FAUNA AND AGE OF SAMPLES FROM THE WIDE BAY-OPEN BAY AREA, EAST NEW BRITAIN. Records 1968/82
THE FORAMINIFERAL FAUNA AND AGE OF SAMPLES FROM THE WIDE BAY-OPEN BAY AREA, EAST NEW BRITAIN by D.J. Belford Records 1968/82 The information contained in this report has been obtained by the Department
More informationState the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks.
Objectives State the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks. Compare three types of unconformities. Apply the law of crosscutting
More informationSedimentiogical study for subsurface section of Abu Khasib
Journal of Genetic and Environmental Resources Conservation, 2013,1(2):79-83. www.jgerc.com Sedimentiogical study for subsurface section of Abu Khasib Sadi K. Jan Iraq Natural History Research Center and
More informationArthur Saller 1. Search and Discovery Article #51393 (2017)** Posted June 26, Abstract
PS Mixed Carbonates and Siliciclastics North of the Mahakam Delta, Offshore East Kalimantan, Indonesia* Arthur Saller 1 Search and Discovery Article #51393 (2017)** Posted June 26, 2017 *Adapted from poster
More informationGY 112L Earth History
GY 112L Earth History Lab 2 Vertical Successions and Sequences of Events GY 112L Instructors: Douglas Haywick, James Connors, Mary Anne Connors Department of Earth Sciences, University of South Alabama
More information19 00' N 70 20' W Loma La Cuaba volcanic edifice 70 00' W Pueblo Viejo District (location of Fig. 2) Loma Navisa volcanic edifice 69 40' W & S a m a n á B a y 0 10 20 Kilometers 18 50' N Guaimarote Hatillo
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 14: Sedimentary Rocks Part 2: Alluvial Fans and Rivers Instructor: Dr. Douglas W. Haywick Last Time 1) Types of Sediment 2) Sedimentary Rock
More informationTopographic map analysis to determine Arjuno-Welirang volcanostratigraphy and implication for geothermal exploration
IOP Conference Series: Earth and Environmental Science PAPER OPEN ACCESS Topographic map analysis to determine Arjuno-Welirang volcanostratigraphy and implication for geothermal exploration To cite this
More informationDepositional Environment and Sequence Stratigraphy of the Neocomian Fahliyan Formation in North Dezful Embayment, Iran
Depositional Environment and Sequence Stratigraphy of the Neocomian Fahliyan Formation in North Dezful Embayment, Iran Mostafa Sabouhi 1*, Davood Jahani 2, Farid Taati Qurayem 3 and Ali Aminzadeh 4 *1
More informationJAPEX s 60 Years Experience Exploring Volcanic Reservoirs in Japan*
Click to view oral presentation (3.00 MB) JAPEX s 60 Years Experience Exploring Volcanic Reservoirs in Japan* Kentaro Takeda 1 and Yasuo Yamada 2 Search and Discovery Article #70297 (2017)** Posted October
More informationGLY 155 Introduction to Physical Geology, W. Altermann. Press & Siever, compressive forces. Compressive forces cause folding and faulting.
Press & Siever, 1995 compressive forces Compressive forces cause folding and faulting. faults 1 Uplift is followed by erosion, which creates new horizontal surface. lava flows Volcanic eruptions cover
More informationHYDRO-CHEMICAL AND STABLE ISOTOPE PROPERTIES OF GROUNDWATER IN MT. KARANG, WEST JAVA, INDONESIA
HYDRO-CHEMICAL AND STABLE ISOTOPE PROPERTIES OF GROUNDWATER IN MT. KARANG, WEST JAVA, INDONESIA Boy Yoseph CSS SYAH ALAM1, Ryuichi ITOI2 and Sachihiro TAGUCHI3 1 2 Facultyof Geology, Padjadjaran University,
More informationBefore Plate Tectonics: Theory of Continental Drift
Before Plate Tectonics: Theory of Continental Drift Predecessor to modern plate tectonics Shape and fit of the continents was the initial evidence Snider-Pelligrini (1858) Taylor (1908) Wegner (1915) Fig.
More informationUnderstanding Earth Fifth Edition
Understanding Earth Fifth Edition Grotzinger Jordan Press Siever Chapter 5: SEDIMENTATION: Rocks Formed by Surface Processes Lecturer: H Mohammadzadeh Assistant professors, Department of Geology, FUM Copyright
More informationGEOLOGY MEDIA SUITE Chapter 8
UNDERSTANDING EARTH, SIXTH EDITION GROTZINGER JORDAN GEOLOGY MEDIA SUITE Chapter 8 Clocks in Rocks Timing the Geologic Record 2010 W.H. Freeman and Company Stratigraphy and fossils Figure 8.4 (page 172)
More informationInterpretation of Subsurface Geological Structure of Massepe Geothermal Area Using Resistivity Data
Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Interpretation of Subsurface Geological Structure of Massepe Geothermal Area Using Resistivity Data Ahmad Zarkasyi and Yuanno
More informationThe Lithosphere and the Tectonic System. The Structure of the Earth. Temperature 3000º ºC. Mantle
The Lithosphere and the Tectonic System Objectives: Understand the structure of the planet Earth Review the geologic timescale as a point of reference for the history of the Earth Examine the major relief
More informationGEOLOGY MEDIA SUITE Chapter 5
UNDERSTANDING EARTH, SIXTH EDITION GROTZINGER JORDAN GEOLOGY MEDIA SUITE Chapter 5 Sedimentation Rocks Formed by Surface Processes 2010 W.H. Freeman and Company Mineralogy of sandstones Key Figure 5.12
More informationL.O: HOW GEOLOGISTS SEQUENCE EVENTS IN EARTH'S GEOLOGIC HISTORY IF NOT OVERTURNED, OLDEST ON BOTTOM, YOUNGEST ON TOP
L.O: HOW GEOLOGISTS SEQUENCE EVENTS IN EARTH'S GEOLOGIC HISTORY IF NOT OVERTURNED, OLDEST ON BOTTOM, YOUNGEST ON TOP 1. Unless a series of sedimentary rock layers has been overturned, the bottom rock layer
More informationIdentifying the Distribution of Alteration Zone Using Very Low Frequency Method in Candi Gedong Songo, Ungaran, Semarang, Central Java
IOP Conference Series: Earth and Environmental Science PAPER OPEN ACCESS Identifying the Distribution of Alteration Zone Using Very Low Frequency Method in Candi Gedong Songo, Ungaran, Semarang, Central
More informationPlay fairway mapping in the Northeast Atlantic Margin Comparison between mature and immature basins. David Mudge, Joanne Cranswick
Play fairway mapping in the Northeast Atlantic Margin Comparison between mature and immature basins David Mudge, Joanne Cranswick Contents Ternan North Sea Play fairway mapping Tertiary case study Northeast
More informationPacific Northwest Rock Lab, Part II. Igneous Rocks. Name Per.
Name Per. Pacific Northwest Rock Lab, Part II After you ve classified all your rocks, place their numbers next to the names and read the information about the rock. Check the classifications here (igneous,
More informationConceptual model of groundwater and river water interactions in Cikapundung riverbank, Bandung, West Java
IOP Conference Series: Earth and Environmental Science OPEN ACCESS Conceptual model of groundwater and river water interactions in Cikapundung riverbank, Bandung, West Java To cite this article: Achmad
More informationChapter 10. Chapter Rocks and the Rock Cycle. Rocks. Section 1 Rocks and the Rock Cycle
Chapter 10 Rocks 1 Chapter 10 Section 1 Rocks and the Rock Cycle 2 10.1 Rocks and the Rock Cycle Magma is the parent material for all rocks. Once the magma cools and hardens, many changes can occur. Geology:
More informationRockall Plateau. OCN 201: Shelf Sediments
Rockall Plateau OCN 201: Shelf Sediments Classification by Size Classification by Mode of Formation Detrital sediments Transported and deposited as particles Derived from weathering of pre-existing rocks
More informationAnswers: Internal Processes and Structures (Isostasy)
Answers: Internal Processes and Structures (Isostasy) 1. Analyse the adjustment of the crust to changes in loads associated with volcanism, mountain building, erosion, and glaciation by using the concept
More informationPaleoenvironmental Study of Miocene Sediments from JTB-1 and NRM-1 wells, in West Ogan Komering Block, Meraksa Area, South Sumatra Basin
IOP Conference Series: Earth and Environmental Science PAPER OPEN ACCESS Paleoenvironmental Study of Miocene Sediments from JTB-1 and NRM-1 wells, in West Ogan Komering Block, Meraksa Area, South Sumatra
More informationMicrofacies and Sedimentary Environments of the Fahliyan Formation in the Folded Zagros Zone, SW Iran
International Journal of Advances in Applied Sciences (IJAAS) Vol. 2, No. 1, March 2013, pp. 51~58 ISSN: 2252-8814 51 Microfacies and Sedimentary Environments of the Fahliyan Formation in the Folded Zagros
More informationGEOLOGIC MAPS AND GEOLOGIC STRUCTURES A TEXAS EXAMPLE
GEOLOGIC MAPS AND GEOLOGIC STRUCTURES A TEXAS EXAMPLE Roger Steinberg Assistant Professor of Geology Del Mar College 101 Baldwin Corpus Christi, TX 78404 361-698-1665 rsteinb@delmar.edu For the maps accompanying
More informationSYNOPSIS SUBMITTED TO RASHTRASANT TUKADOJI MAHARAJ NAGPUR UNIVERSITY, NAGPUR FOR THE DEGREE OF DOCTOR OF PHILOSOPHY
SEDIMENTOLOGY AND PALEOALGOLOGY OF THE CENOZOIC SEDIMENTS OF KACHCHH OFFSHORE BASIN, INDIA: SIGNIFICANCE IN RECONSTRUCTION OF PALEOENVIRONMENTS AND HYDROCARBON EXPLORATION SYNOPSIS SUBMITTED TO RASHTRASANT
More information