Upload
others
View
0
Download
0
Embed Size (px)
Citation preview
Prosiding Semnas SINTA FT UNILA Vol. 1 Tahun 2018
Riset PT-Eksplorasi Hulu Demi Hilirisasi Produk
Bandar Lampung, 19 Oktober 2018
ISBN: 2655-2914
-------------------------------------------------------------------------------------------------------------------------------------------------------------------------------
© Fakultas Teknik Universitas Lampung - 198 -
Sedimentological Study of Ngrayong Formation at Candi and Surrounding Area, Todanan
Blora, Central Java
Rezky Aditiyo1 , Djuhaeni2
, Bambang Priadi2 , Supriyanto 1,* 1University of Indonesia, Gedung A FMIPA UI, Beji, Kota Depok, Jawa Barat 16424.
2 Bandung Institute of Technology, Teknik Geologi, Jalan Ganeca 10, Bandung, Jawa Barat 40132
*Corresponding Author: [email protected]
Abstract. Research area is located on Candi Village, Todanan District, Blora Regency, Central Java, which is
geographically 111010’30” – 110012’00” LS dan 6052’42” – 6055’00” BT. The area is about 12 km2. Stratigraphy unit
consists of four stratigraphy units. Tawun Formation claystone Unit was deposited on the late of Early Miocene. Ngrayong
sandstone Unit was lying on it, deposited conformably on the early of Middle Miocene. Then on the late of Middle Miocene
until the early of Late Miocene, Bulu Formation limestone Unit was deposited unconformably on middle neritic until outer
neritic environment. Wonocolo Formation Marl Unit, then deposited on the Late Miocene. Geological structure found
were anticline and strike slip fault, had been developed by N-S tectonic force since Pliocene until Pleistocene with a NW–
SE and NE-SW trend. Uplift and erosional process then created nowadays morphology. Ngrayong Formation consists of
quartz sandstone, claystone, and also limestone, divided by three parts, there are: Lower Ngrayong Formation, Middle
Ngrayong Formation, and Upper Ngrayong Formation. Grain size indicating shallow marine facies (surfzone-offshore),
paleontology analysis shows that deep water fossils and shallow marine fossils were mixed together, and also cruziana
trace fossil. Microcline were found in petrography analysis in quartz sand. Based on facies association, Ngrayong
Formation in Candi Area was being interpreted as shallow marine deposition in littoral to inner neritic zone.and
sedimentational pattern and grain size analysis show Ngrayong Formation on Candi area obviously was deposited on
littoral until inner neritic zone. Deep marine fossils that were mixed in shallow marine association were interpreted as
reworked fossils that came from Tuban Formation below Tawun and Ngrayong Formation.
Kata kunci: Ngrayong, Candi, Stratigraphy.
INTRODUCTION
Research area is located on Candi Village, Todanan District, Blora Regency, Central Java, which is geographically
111010’30” – 110012’00” LS dan 6052’42” – 6055’00” BT. It covers an area of approximately ± 12 km2 (Figure 1).
The East Java Basin is situated on the southern margin of the stable Sunda craton and covers an area of approximately
50,000 sq km (Mudjiono and Pireno,, 2001). The Tertiary stratigraphic record of the East Java Basin suggests periods
of relative quiescence alternating with periods of tectonic activity (Simo, et al., 2012). In the Middle Miocene, a
regression phase occurs due to uplift that covering a large area in Indonesia. Uplift causes the quartz-sandstones with
coal layer intercalation and gypsum, Ngrayong Formation, was exposed. This formation was deposited in fluvial (non-
marine) environments, tidal areas to middle neritic.
Figure 1. Administrative map of Central Java Province. Research area are shown with purple rectangle
Stratigraphy unit of the study area consists of four stratigraphy units. Tawun Formation claystone Unit was
deposited on the late of Early Miocene. Ngrayong Formation Unit was deposited conformably on the early of Middle
Miocene. Then on the late of Middle Miocene until the early of Late Miocene, Bulu Formation limestone Unit was
deposited unconformably on middle neritic to outer neritic environment. Wonocolo Formation Marl Unit, the younger
unit, deposited on the Late Miocene. Geological structure found were anticline and strike-slip fault, had been
developed by N-S tectonic force since Pliocene until Pleistocene with a NW–SE and NE-SW trend. Uplift and the
erosional process then created nowadays morphology. The geomorphology unit comprises Anticline Hill Unit,
Hogback Ridge Unit, and Homocline Valley Unit.
Prosiding Semnas SINTA FT UNILA Vol. 1 Tahun 2018
Riset PT-Eksplorasi Hulu Demi Hilirisasi Produk
Bandar Lampung, 19 Oktober 2018
ISBN: 2655-2914
-------------------------------------------------------------------------------------------------------------------------------------------------------------------------------
© Fakultas Teknik Universitas Lampung - 199 -
Figure 2. General stratigraphy of research area. Early Miocene Tawun Formation are the oldest formation can be
recognized, while Late Mioccene Wonocolo Formation are the youngest that are exposed
The Ngrayong Formation was subject to be questioned to who have been working in the East Java Basin, especially
on Cepu, including Candi area. The opinion was about differences in the depositional environment between Ngrayong
as shelf and Ngrayong as deepwater/deep marine sediment. Previous field based study showed that Ngrayong
Formation was deposited on beach – tidal deposit (Poedjoprajitno and Djuhaeni, 2006). Contrary to Ardhana (1993),
Ngrayong Formation was deposited on shelf to submarine fan. This study was therefore conducted to investigate the
depositional environment of The Ngrayong Formation, based on field investigations involving grain size analysis,
petrographic analysis, micropaleontological analysis, and facies analysis.
RESEARCH METHODS
This research is based on field investigations involving facies analysis, grain size analysis, petrographic analysis, and
micropaleontological analysis. Lithofacies, fossils, and grain size analysis can produce comprehensive data of facies
associations that can reflect a certain depositional environment. Relative position stratigraphically from existing data
can provide information for interpretation Ngrayong depositional environment changes. Based on the analysis of
Ngrayong Formation on Candi Village and its surroundings, the author divided Ngrayong Formation based on its
facies association: Lower Ngrayong Formation, Middle Ngrayong Formation, and Upper Ngrayong Formation.
Grain size analysis sampling method was taken from outcrop of quartz-sandstone in the study area. If the outcrop
has a vertical extent stratigraphically more than one meter, sampling was carried out for each meter. Total fifteen
samples were taken for grain size analysis Petrographic analysis was carried out to determine the composition, texture,
type of porosity, and fossils content. Micropaleontology analysis was conducted to determine foraminifera
microfossils that will be used for interpretation of Biozone Zonation (Blow, 1969) and depositional environments
(Tipsword, 1966).
RESULTS AND DISCUSSION
Ngrayong Formation is characterized by quartz-sandstone with predominantly non-carbonated quartz fragment, good
sorting, grain shape angular - subangular, closed fabric, good porosity, easy squeezed, very fine sand - fine sand;
intercalated with limestone and claystone on the lower part, then become limestone dominant on the upper part.
Ngrayong quartz sandstone in the study area develops from the upper part of the Tawun Formation and the middle to
upper part of the Ngrayong Formation.
Based on the analysis of Ngrayong Formation in the Candi area and surrounding area, the author divides Ngrayong
Formation into three parts based on the facies association : Lower Ngrayong Formaition, Middle Ngrayong
Formation, and Upper Ngrayong Formation. Detailed stratigrapy are shown in Figure 3.
Lower Ngrayong Formation
The lithological characteristics of the Lower Ngrayong Formation consist of quartz sand, followed by clastic limestone
at the upper part. quartz-sand has the characteristics of low cemented quartz fragments dominant (loose sand), reddish-
white, non-carbonated, good sorting, subrounded-rounded grain shape, good porosity, fine sand-medium sand, mineral
content consisting of quartz and microcline (Figure). there were some root fossils identified in sand-quartz outcrops
Prosiding Semnas SINTA FT UNILA Vol. 1 Tahun 2018
Riset PT-Eksplorasi Hulu Demi Hilirisasi Produk
Bandar Lampung, 19 Oktober 2018
ISBN: 2655-2914
-------------------------------------------------------------------------------------------------------------------------------------------------------------------------------
© Fakultas Teknik Universitas Lampung - 200 -
in the south of the Candi Village. The sandstone is clean sand with very little cement content, so that its textural
maturity of rocks are mature - super mature. This can be classified as Quartz Arenite. Thin section analysis show
clastic texture, well sorted, closed fabric, long contact, mineral content consist of quartz, plagioclase; very fine sand -
fine sand (0.015-0.25mm), subangular-angular grain shape, and intergranular porosity.
Based on limestone outcrops observation at the R1C location around Ngampel Village, Glauconitic Foraminifera
Packstone is reddish-white, clastic texture, poorly sorted, open fabric, consists of fossil fragments of foraminifera,
intact and cracked form, and siliciclastic in the form of quartz, glauconite with a size of 0.1-1 mm. The matrix consists
of carbonate mud and cement consists of calcite sparry. Porosity types are interparticle and intraparticle.
Figure 3. Detailed stratigraphy of Ngrayong Formation, integrating facies, fossils, and grain size analysis, shows
litoral – inner neritic depositional environment association
Figure 4. Quartz arenite was recognized from R6I sample. Quartz dominant and minor plagioclase and microcline
(D3). Sometimes overgrowth secondary quartz are found
0 0,5 mm 0,5 mm 0
Prosiding Semnas SINTA FT UNILA Vol. 1 Tahun 2018
Riset PT-Eksplorasi Hulu Demi Hilirisasi Produk
Bandar Lampung, 19 Oktober 2018
ISBN: 2655-2914
-------------------------------------------------------------------------------------------------------------------------------------------------------------------------------
© Fakultas Teknik Universitas Lampung - 201 -
Based on grain size analysis of three quartz sand samples, is known that the three samples were deposited in the
surfzone or near shore depositional environment. Deposition mechanisms in this zone can be seen in the graph that
the traction flow is more involved rather than the suspension current mechanism. Graph lines in the traction population
(rolling/sliding and saltation) is not too gentle qualitatively, indicating that sorting is quite good on the deposition of
sand-quartz. Association of Lower Ngrayong Formation shows littoral zone to the edge neritic depositional
envvironment.
Middle Ngrayong Formation
The lithological characteristics are clastic limestone and claystone at the bottom, then quartz sand with clastic
limestone and intercalated claystone on the upper part. Quartz sand with gray-white color, non-carbonate, good
sorting, subrounded-rounded, closed fabric, fine to medium sand, dominant minerals are loose quartz minerals with
few microcline. Reddish-white clastic limestone, medium sorting, angular-subrounded, opened fabric, medium sand-
coarse sand. Claystone with gray color, compact, very fine grained. Vertical succession shows a coarsening upward
pattern.
A thin section of sand-quartz called quartz arenite has characteristic clastic texture, well sorted, closed container,
grain contact long contact, consisting of quartz, plagioclase, very fine sand-fine sand (0.015-0.25mm), subangular-
angular, intergranular porosity.
Foraminifera wackestone has clastic texture, poorly sorted, opened fabric, consisting of foraminifera fragments
(Lepidocylina, Katacyclopeus annulus, Amphistegina sp.), medium sand-fine sand (0.2-0.9mm), rounded-angular
grain shape. The matrix consist of micrite. Cements are sparry calcite. Porosity are Interparticles and moldic.
Micropaleontological analysis on Middle Ngrayong Sandstone represented by R6J samples showed the presence
of Quinqueloculina sp., Operculina sp., Rotalia sp., and Elphidium sp., showing association of littoral - middle neritic
environment. Grain size analysis on Middle Ngrayong Sandstone section was carried out on twelve quartz sand
samples. Stratigraphically, it was interpreted that there is a change from the lower shoreface to foreshore and surfzone.
Based on the facies association, Middle Ngrayong Formation was deposited in edge neritic environment.
Upper Ngrayong Formation
The Upper Ngrayong Formation consist of clastic limestones intercalated with sandstone and claystone, showing
coarsening upwards succession. Clastic limestone has clastic texture, poor sorting, subangular-subrounded, opened
fabric, medium porosity, compact, contains fossils such as Lepidocyclina sp., red algae, and Katacycloclypeus
annulatus. Claystone has a gray color, carbonate, rarely intercalated with sandstone with Brachiopods shell fragments,
Turritella sp., foraminifera, and pyrite minerals. Clastic limestone has the characteristics of gray-white color,
sometimes sandy, poorly sorted, subangular-subrounded, medium sand-coarse sand. Foraminifera are
Katacycloclypeus annulatus, Lepidocyclina sp., and Amphistegina sp. While sandstones has a grayish-black color,
medium sorting, opened fabric, fine sand-coarse sand, compact, fragments consists of mineral quartz, mica, and shell
fragments.
Benthic foraminifers in R3E, R5D, and R5C samples were observed along with their bathymetry (Tipsword, 1966)
are Cibicides sp. (middle neritic), Quinqueloculina sp. (littoral), and Elphidium sp. (edge neritic) in R3E sample.
Quinqueloculina sp. (littoral) and Rotalia sp. (littoral) in the R5D sample, then Cibicides sp. (middle neritic),
Operculina sp. (middle neritic), and Elphidium sp. ( edge neritic) in the sample R5C. Whereas in the R3C sample can
be observed benthonic foraminifera such as Gyroidina sp. (upper bathyal), Operculina sp. (middle neritic),
Quinqueloculina sp. (littoral), Elphidium sp. (edge neritic), and Bolivina sp. (outer neritic). Then in the R3A sample
shows the presence of Cibicides sp. and Bolivina sp. cruziana fossils were also found. Cruziana indicates the offshore
environment.
Deep marine benthonic foraminifera were found in shallow marine fossils association. This was interpreted as a
reworked fossils. Depositional sequences from Tawun Formation to the Wonocolo Formation show the transgressive
depositional series. Facies association of shallow marine deposits of Ngrayong Formation, indicates that a certain
sedimentation processes occurs which made deep marine fossils mixed with shallow marine fossils association. Deep
marine fossils were interpreted as reworked fossils from Tuban Formation that was deposited on Early Miocene on
deep marine setting. Based on the comprehensive data described earlier, it can be concluded that Ngrayong Formation
in Candi area and its surroundings are deposited in the littoral zone to the edge neritic.
Prosiding Semnas SINTA FT UNILA Vol. 1 Tahun 2018
Riset PT-Eksplorasi Hulu Demi Hilirisasi Produk
Bandar Lampung, 19 Oktober 2018
ISBN: 2655-2914
-------------------------------------------------------------------------------------------------------------------------------------------------------------------------------
© Fakultas Teknik Universitas Lampung - 202 -
Figure 5. Summary of Micropaleontogy analysis. Foraminifera associations show deepening upward trend from
Tawun to Wonocolo Formation. O : rare (1-3); + : few (4-10); | : common (11-25); -: barren
CONCLUSION
Ngrayong Formation could be divided to three parts based on facies association, there are Lower Ngrayong Formation,
Middle Ngrayong Formation, and Upper Ngrayong Formation. Based on lithological characteristic, grain size analysis,
petrography, and microfossils analysis, it can be concluded that Ngrayong Formation in Candi and its surrounding
area was deposited at shallow marine from litoral to inner neritic zone. Deep marine fossils in shallow marine fossils
association were interpreted as reworked fossils from older formation (Tuban Formation).
transisi
neritik pinggir
neritik tengah
neritik luar
batial atas
N14
R2
BG
lob
oro
talia
men
ard
ii+
OO
+I
O+
O+
OO
N13
R2
AG
lob
oro
talia
foh
siI
+O
++
OO
OI
+O
O
N12
R3
AG
lob
oro
talia
foh
si+
++
O+
O
R3
EO
+O
+I
+
N9
R6
JO
rbu
lina
un
iversa+
IO
+I
O+
O
R1
B-
-R
1A
--
Cassidulina sp.
Miosen Tengah Miosen Tengah Miosen Akhir
R3
C
R5
C
Batugamping
Formasi
I
Ngrayong
I
I
I
I
O
+
+
Globigerinoides obliquus
Globigerinoides trilobus immaturus
Globorotalia obesa I
Globoquadrina altispira
Globoquadrina dehiscens
I
Spesies Index
Orbulina suturalis
O
Globigerinoides trilobus trilobus
Globigerinoides sacculifer
+
I
I
I
I
OG
lob
oro
talia
aco
staen
sis R
2C
I
R5
D
+
I
O
Oolina sp.
I
Elphidium sp.
+
Bolivina sp.
O
I
I
O O
Nodosaria spp.
Globorotalia acostaensis
Gyroidina sp.
Rotalia sp.
Operculina sp.
Kelimpahan Foraminifera Benthonik
Nonion sp.
Bulimina sp.
Quinqueloculina sp.
Cibicides sp.
Texturalia sp.
O O
O
O
O
I
Amphistegina lessonii
+
I
Uvigerina sp.
I
+
Umur
Zonasi Planktonik (Blow, 1979)
Globigerina praebulloides
Globigerina bulloides
Orbulina universa
Globorotalia fohsi
Lingku
nga
n p
engen
da
pa
n
Kelimpahan foraminifera planktonik
I
I
Satuan batuan
Lokasi sampel
+ I
I
O OIO
R4
J
R4
K
R7
E
I
I
+
I
II
Napal
+I
I
I
+
+
+O
O
+I
+
I
+
Tawun Wonocolo
Batupasir
Globogerinoides subquadratus
+ I
Globrotalia menardii
Batulempung
Glo
big
erina
pra
ebu
lloid
es
Bulu
+
N10-N11 N 17N16
O
Prosiding Semnas SINTA FT UNILA Vol. 1 Tahun 2018
Riset PT-Eksplorasi Hulu Demi Hilirisasi Produk
Bandar Lampung, 19 Oktober 2018
ISBN: 2655-2914
-------------------------------------------------------------------------------------------------------------------------------------------------------------------------------
© Fakultas Teknik Universitas Lampung - 203 -
ACKNOWLEDGEMENT
We would like to thank Faculty Member of Mathematics and Natural Sciences University of Indonesia. Special
appreciation for Dr. Djuhaeni and Dr. Bambang Priadi (Geology Department of Institut Teknologi Bandung) for great
technical discussions.
REFERENCES
Ardhana, W. 1993. A Depositional Model for The Early Miocene Ngrayong Formation and Implication for
Exploration in The East Java Basin. Jakarta: 22nd IPA Proceedings.
Blow, W. H., 1969. Late Miocene to Recent planktonic foraminifera biostratigraphy: In Brönnimann, P. and Renz, H.
H. (eds.), Proceedings First Int. Conf. on planktonic microfossils, Geneva, 1967, v. 1, pp. 199-422.
Mudjiono, R. and Pireno, G.E.. 2001. Exploration Of The North Madura Platform, Offshore East Java, Indonesia.
Jakarta: 28th IPA Convention & Exhibition Proceedings.
Simo, T., Sekti, Rizki P., Hakiki, F., Sun, M., Myers., R. Fullmer., S. 2012. Reservoir Characterization and Simulation
of an Oligocene-Miocene Isolated Carbonate Platform: Banyu Urip Field, East Java Basin, Indonesia. Search and
Discovery Article.
Soedjoprajitno, S and Djuhaeni. (2006). Unit Genesa Pasir Ngrayong di Desa Ngepon Jatim, Cekungan Jawa Timur
Utara. 38th Geologi Bulletin.
Tipsword, H. L., F. M. Setzer, and F. L. Smith, Jr.. 1966. Interpretation of depositional environment in Gulf Coast
petroleum exploration from paleoecology and related stratigraphy: Transactions of the Gulf Coast Association of
Geological Societies, vol. 16, p. 119–130.