DAFTAR PUSTAKA
Aitken, J. F. dan Flint, S. S., 1995. The Application of High Resolution Sequence Stratigraphy to Fluvial Systems: A Case Study from the Upper Caboniferous Breathitt Group, Eastern Kentucky: Sedimentology, v. 42, 193 – 206. Allen, G. P. dan Posamentier, H. W., 1993. Sequence Stratigraphy and Facies Model of an Incised Velley Complexes: the Gironde Estuary, France: Journal of Sedimentary Petrology, v. 63, 378 – 391. Aswan, 2007. Shell Beds Taphonomic Study and Its Implication for Depositional Setting Analysis, Ceramah Ilmiah Pusat Survey Geologi Bandung. Aswan dan Ozawa, T., 2006. Middle Miocene Milankovitch 41.000-year Cycles Interpretation Based on Molluscs Fossils Association and Lithofacies in Tropical Sediments,
Nyalindung
Formation,
Sukabumi,
West
Java,
Indonesia.
Paleogeography, Paleoclimatology, Paleoecology 235, 382-405. Aswan, Zaim, Y. dan Rizal, Y., 2006. Distribution of Quarternary Freshwater Molluscs Fossils in Jawa dalam buku: S. Sartono: Dari Hominid ke Delapsi dengan Kontroversi, Penerbit ITB, 109-120. Bartov, Y., Stein, M., Enzel, Y., Agnon, A. dan Rechez, Z., 2000. Lake Levels and Sequence Stratigraphy of Lake Lisan, the Late Pleistocene Precursos of the Dead Sea, Quarternaty Research 57, 9 – 21. Boggs, S. Jr., 1992. Petrology of Sedimentary Rocks, Macmillan Publishing Company, New York, 304-352. Butterworth, P. dan Wain, T., 1993. Sedimentology of Karbindo Coal Mine (tidak dipublikasikan). Cantalamessa, G., Di Celma, C. dan Ragaini, L., 2004. Sequence Stratigraphy Of The Punta Ballena Member Of The Jama Formation (Early Pleistocene, Ecuador): Insights from Integrated Sedimentologic, Taphonomic and Paleoecologic Analysis
of
Molluscan
Shell
Concentrations,
Palaeoclimatology, Palaeoecology 216 (2005), 1 – 25.
Palaeogeography,
Coster, G.L. de., 1974. The Geology of The Central and Sumatera Basin: Proc. 3rd Ann. Conv. IPA, Jakarta, 77-110. Darman, H. dan Sidi, F.H. 2000. An Outline of The Geology of Indonesia, IAGI, 11-33. Eubank, R.T. dan Makki, A.C., 1981. Structural Geology of The Central Sumatera Back-Arc Basin, Proceeding IPA, Tenth Annual Convention, 153-196. Gafoer, S., 2002. Tatanama Stratigrafi Graben Kiliran Sebagai Cekungan Terpisah Paleogen Awal Daerah Sumatra Barat: Proc. Ilmiah Sehari Ungkapan Syukur Atas Karya-Karya dan Pengabdian Prof. Dr. R. P. Koesoemadinata, 27-45. Haq, B. U., Hardenbol, J., dan Vail, P. R., 1987. Chronology of Fluctuating Sea Levels Since The Triassic: Science, v.235, 1156-1167. Heidrick, T. L. dan Aulia, K., 1993. A Structural and Tectonic Model of The Coastal plains Block Central Sumatara Basin Indonesia: Proc. 22nd Ann. Conv.As. IPA, 285-304. Heidrick, T. L. dan Aulia, K., 1996. Regional Structural Geology, Chapter II. Petroleum Geology of the Central Sumatra Basin, BPPKA/Pertamina, Jakarta, Indonesia, 13 – 156. Heidrick, T. L., Yarmanto, Indrawardana dan Strong, B. L., 1995. Tertiary Tectonostratigraphic Development of The Balam Depocenter, Central Sumatra Basin Indonesia: Proc. 24th Ann. Conv. IPA, 33-45. Jervey, M. T., 1988. Quantitative Geological Modeling of Siliclastic Rock Sequences and Their Seismic Expression, pada Wilgus, C. K. , Hastings, B. S., Kendall, C. G. St. C., Posamentier, H. W., Ross, C. A. dan van Wagoner, J. C., eds., SeaLevel Changes – An Integrated Approach; Society of Economic Paleontologist and Mineralogists Special Publication No. 42, 47 – 40. Katz, B. J. dan Dawson, W. C., 1997. Pematang - Sihapas Petroleum System of Central Sumatra. pada Proceedings of an International Conference on Petroleum Systems of S. E. Asia and Australasia (Ed. Howes, J. V. C. and Noble, R. A.), 685 - 698.
Keighley, D., Flint, S., Howell, J. dan Moscariello, A., 2003. Sequence Stratigraphy In Lacustrine Basins: A Model For Part Of The Green River Formation (Eocene) Southwest Uinta Basin, Utah, U.S.A: Journal of Sedimentary Research, Vol. 73, No. 6, November, 2003, 987–1006. Kim, W. dan Paola, C., 2007. Long-period Cyclic Sedimentation with Constant Tectonic Forcing in An Experimental Relay Ramp pada Geology; April 2007; v. 35; Geological Society of America; 331 – 334. Kitamura, A., Kondo, Y., Sakai, H. dan Horii, M., 1994. 41,000 Year Orbital Obliquity Expressed as Cyclic Changes in Lithofacies and Molluscan Content, Early Pleistocene Omma Formation, Central Japan, Paleogeography, Paleoclimatology, Paleoecology 112, 345 – 361. Koesoemadinata, R. P., 1985. Prinsip-Prinsip Sedimentasi, Jurusan Teknik Geologi, Institut Teknologi Bandung. Koning, T., 1985. Petroleum Geology of The Ombilin Intermontane Basin, West Sumatra pada Proceedings Indonesian Petroleum Association, 14th Annual Convention, October 1985, 117 – 137. Lee, R. A., 1982. Petroleum Geology of The Malacca Strait Contract Area (Central Sumatra Basin): Proc. 11th Ann. Conv. IPA, 243-263. Longstaffe, F. J., 1981. Short Course in Clays and the Resource Geologist, Mineralogical Association of Canada. Martodjojo, S., Djuhaeni, 1996. Sandi Stratigrafi Indonesia, Ikatan Ahli Geologi Indonesia. Moertosono, S., dan Nayoan, G. As., 1974. The Tertiary Basinal Area of Central Sumatera: Proc. 3rd Ann. Conv. IPA, 63-76. Parras, A., dan Casadío, S., 2004. Taphonomy and sequence Stratigraphic Significance of Oyster-dominated Concentrations from the San Julián Formation, Oligocene of Patagonia, Argentina, Palaeogeography, Palaeoclimatology, Palaeoecology 217 (2005), 47 – 66.
Posamentier, H. W. dan Vail, P. R., 1988. Eustatic Controls on Clastic Deposition II – Sequence and Systems Tract Models, pada Wilgus, C. K., Hastings, B. S., Kendall, C. G. St. C., Posamentier, H.W., Ross, C. A., dan van Wagoner, J. C., eds., Sea-Level Changes – An Integrated Approach, Society of Economic Paleontologists and Mineralogists Special Publication No. 42, 109 – 124. Posamentier, H. W., Jervey, M. T. dan Vail, P. R., 1988. Eustatic Controls on Clastic Deposition I – Conceptual Framework, pada Wilgus, C. K., Hastings, B. S., Kendall, C. G. St. C., Posamentier, H.W., Ross, C. A., dan van Wagoner, J. C., eds., Sea-Level Changes – An Integrated Approach, Society of Economic Paleontologists and Mineralogists Special Publication No. 42, 125 – 154. Pulunggono, A., dan Cameron, N. R., 1984. Sumatran Microplates, Their Characteristics and Their Role in The Evolution of The Central and South Sumateran Basin: 13th Ann. Conv. IPA, 121-129. Rutten, L.M.R., 1927, Voordrachten Over de Geologic van Nederlands Cost Indie: WOLTERS, U.M., Groningen - Den Haag. Shipman, P., 1981. Life History of A Fossil: An Introduction to Taphonomy and Paleoecology, Harvard University Press. Smith, G. I., Benson, L. V. dan Currey, D. R., 1989. Quaternary Geology of the Great Basin 28th International Geological Congress Guidebook, T117, American Geophysical Union, Washington, DC, 78 Sturm, M., Vologina, E. G., Baster, I., Sinnet, B., Mackay, A. W., Ryves, D., 2003. Recent Sedimentation in Lake Baikal, Geophysical Research Abstracts, Vol. 5, 02822, European Geophysical Society. Van Wagoner, J.C., Posamentier, H.W., Mitchum, R.M., Vail, P.R., Sarg, J.F., Loutit, T.S., Hardenbol, J., 1988. An Overview Of Sequence Stratigraphy And Key Definitions: Wilgus, C.W., et al., (Eds.), Sea Level Changes: An Integrated Approach, Special Publication-Society of Economic Paleontologists and Mineralogists, vol. 42, 39 – 45.
Walker, R. G. dan Bhattacharya, J. P., 1992. Deltas, pada Walker, R. G. dan James, P. D., eds., Facies Model: Response to Sea Level Change: Geological Association of Canada, 157 – 179. William, H. H., Kelley, P. A., Janks, J. S., Christensen, R. M., 1985. The Paleogen Rift Basin Source Rock of Central Sumatra: Proc. 14th Ann. Conv. IPA, 57-88. Yarmanto dan Aulia, K., 1989. Seismic Expression of Wrench Tectonics in The Central Sumatra Basin, Journal of Indonesian Association of Geologist (IAGI), Vol. 12. http://deschutes.gso.uri.edu/~rutherfo/milankovitch.html. http://www.homepage.montana.edu/~geol445/hyperglac/time1/milankov.htm, 17 Mei 1999.
LAMPIRAN
Lampiran A-1 Analisis Petrografi No. Conto
:A–2
Satuan Batuan : Batulanau – Serpih
Lokasi
: Pit A
Nama Batuan : Batulanau
Perbesaran P2 (100 kali) A
B
C
D
E
A
B
C
D
E
1
1
1
2
2
2
3
3
3
4
4
4
5
5
5
6
6
6
7
7
7
A
B C D Nikol Sejajar
E
A
B C D Nikol Bersilang 0
mm
E
0,5
Deskripsi Batulanau, tekstur klastik, terpilah baik, kemas tertutup, butiran berupa kalsit (15%), mineral opak (5%), matriks berupa lempung (69%), semen berupa kuarsa (10%), porositas (1%) Kalsit (15%): Sebagai butiran; agak lapuk, berukuran 0,1 – 0,8 mm, agak menyudut (contoh: C3). Mineral Opak (5%): Sebagai butiran; berukuran 0,001-0,05 mm, anhedral (contoh: B4). Lempung (69%): Sebagai matriks; hadir mengikat butiran, berwarna coklat keruh. Kuarsa (10%) Sebagai semen; pemadaman bergelombang, mengisi ruas antar butiran. Porositas (1%)
Lampiran A-2 Analisis Petrografi No. Conto
: A – 11
Satuan Batuan
: Batulanau – Serpih
Lokasi
: Pit A
Nama Batuan
: Batulempung
Perbesaran P2 (100 kali) A
B
C
D
E
A
B
C
D
E
1
1
1
2
2
2
3
3
3
4
4
4
5
5
5
6
6
6
7
7
7
A
B
C
D
Nikol Sejajar
E
A
B
C
D
E
Nikol Bersilang 0
mm
0,5
Deskripsi Batulempung, tekstur klastik, terpilah baik, kemas tertutup, butiran berupa mineral opak (20%), matriks berupa lempung (69%), semen berupa kalsit (10%), porositas (1%) Mineral Opak (20%): Sebagai butiran; berukuran 0,001-0,05 mm, anhedral (contoh: B4). Lempung (69%): Sebagai matriks; hadir mengikat butiran, berwarna coklat keruh. Kalsit (10%) Sebagai semen; berwarna coklat gelap, mengisi ruas antar butiran, bentuk kristal anhedral. Porositas (1%)
Lampiran A-3 Analisis Petrografi No. Conto
: a – 11
Satuan Batuan
: Batulanau – Serpih
Lokasi
: Pit A
Nama Batuan
: Batulempung
Perbesaran P2 (100 kali) A
B
C
D
E
A
B
C
D
E
1
1
1
2
2
2
3
3
3
4
4
4
5
5
5
6
6
6
7
7
7
A
B
C
Nikol Sejajar
D
E
A
B
C
D
E
Nikol Bersilang 0
mm
0,5
Deskripsi Batulempung, tekstur klastik, terpilah baik, kemas tertutup, butiran berupa cangkang moluska (20%), matriks berupa lempung (69%), semen berupa kalsit (10%), porositas (1%) Cangkang Moluska (20%): Sebagai butiran; terdiri dari moluska gastropoda (contoh: C4). Lempung (69%): Sebagai matriks; hadir mengikat butiran, berwarna coklat keruh. Kalsit (10%) Sebagai semen; berwarna coklat gelap, mengisi ruas antar butiran, bentuk kristal anhedral. Porositas (1%)
Lampiran A-4 Analisis Petrografi No. Conto
: E02 – 150
Satuan Batuan
: Batulanau – Serpih
Lokasi
: Pit E
Nama Batuan
: Batulanau
Perbesaran P2 (100 kali) A
B
C
D
E
A
B
C
D
E
1
1
1
2
2
2
3
3
3
4
4
4
5
5
5
6
6
6
7
7
7
A
B
C
Nikol Sejajar
D
E
A
B
C
D
E
Nikol Bersilang 0
mm
0,5
Deskripsi Batulanau, tekstur klastik, terpilah baik, kemas tertutup, butiran berupa kuarsa (5%), material karbon (10%), matriks berupa lempung (74%), semen berupa kuarsa (10%), porositas (1%) Kuarsa (5%): Sebagai butiran; agak lapuk, berukuran 0,02– 0,1 mm, agak menyudut, pemadaman bergelombang. (contoh:C5) Material Karbon (10%): Sebagai butiran (contoh: D6) Lempung (74%): Sebagai matriks; hadir mengikat butiran, berwarna coklat keruh Kuarsa (10%) Sebagai semen; pemadaman bergelombang, mengisi ruas antar butiran Porositas (1%)
Lampiran B Analisis XRD (X-Ray Diffraction) No. Conto
: am – 12
Satuan Batuan
: Batulanau – Serpih
Lokasi
: Pit A
Nama Batuan
: Serpih
File: am–12 .DI 31-Mar-2008 16:10 ===================================================== Philips Analytical X-Ray B.V. Metalurgi-ITB Sample identification: Am-12 Data measured at: 31-Mar-2008 15:38:00 Diffractometer type: PW1710 BASED Tube anode: Cu Generator tension [kV]: 40 Generator current [mA]: 30 Wavelength Alpha1 [Å]: 1.54056 Wavelength Alpha2 [Å]: 1.54439 Intensity ratio (alpha2/alpha1): 0.500 Divergence slit: AUTOMATIC Irradiated length [mm]: 12 Receiving slit: 0.2 Monochromator used: NO Start angle [º2Ø]: 5.010 End angle [º2Ø]: 64.990 Step size [º2Ø]: 0.020 Maximum intensity: 1056.250 Time per step [s]: 0.500 Type of scan: CONTINUOUS Intensities converted to: FIXED Minimum peak tip width: 0.00 Maximum peak tip width: 1.00 Peak base width: 2.00 Minimum significance: 0.75 Number of peaks: 34
Angle d-value d-value Peak width Peak int Back. int Rel. int Signif. [º2Ø] à1 [Å] à2 [Å] [º2Ø] [counts] [counts] [%] ==================================================== 8.775 10.0688 11.690 7.5638 12.445 7.1066 15.580 5.6829 17.800 4.9789 19.900 4.4579 20.945 4.2378 23.220 3.8275 24.935 3.5680 26.730 3.3323 29.430 3.0325 29.545 3.0209 31.335 2.8523 33.145 2.7006 35.055 2.5577 36.055 2.4890 36.585 2.4542 37.765 2.3801 38.555 2.3332 39.570 2.2756 40.335 2.2342 42.605 2.1203 43.270 2.0892 45.865 1.9769 47.610 1.9084 48.620 1.8711 50.210 1.8155 54.975 1.6689 56.340 1.6316 56.835 1.6186 57.450 1.6027 60.015 1.5402 60.825 1.5216 62.375 1.4875
10.0939 7.5826 7.1242 5.6971 4.9912 4.4690 4.2483 3.8370 3.5769 3.3406 3.0400 3.0284 2.8594 2.7073 2.5640 2.4952 2.4603 2.3861 2.3390 2.2813 2.2398 2.1255 2.0944 1.9818 1.9131 1.8757 1.8200 1.6730 1.6357 1.6226 1.6067 1.5440 1.5254 1.4912
0.480 0.120 0.280 0.120 0.240 0.320 0.100 0.200 0.100 0.180 0.100 0.120 0.640 0.160 0.120 0.200 0.200 0.320 0.240 0.160 0.160 0.160 0.160 0.240 0.200 0.200 0.160 0.320 0.120 0.640 0.060 0.200 0.240 0.320
110 428 1056 37 67 161 331 137 471 835 306 331 16 37 66 83 53 46 53 106 19 23 59 29 45 52 58 30 28 12 28 32 9 19
655 437 392 262 216 182 166 146 130 114 100 98 90 79 72 69 66 62 61 58 55 49 48 42 38 37 35 29 28 28 28 27 26 26
10.4 40.6 100.0 3.5 6.4 15.3 31.4 13.0 44.6 79.1 29.0 31.4 1.5 3.5 6.2 7.8 5.0 4.4 5.0 10.0 1.8 2.2 5.6 2.8 4.2 4.9 5.5 2.9 2.7 1.1 2.7 3.1 0.9 1.8
0.80 1.37 6.99 0.76 1.72 1.78 1.33 2.19 0.87 13.43 1.23 2.54 0.95 1.09 0.80 2.32 1.71 1.54 1.45 2.73 0.80 1.0 1.33 1.16 1.44 2.05 2.65 0.93 1.46 1.08 1.17 1.70 0.85 1.54
Lampiran C-1 Analisis Granulometri No. Conto
: am – 2
Satuan Batuan : Batulanau–Serpih
Lokasi
: Pit A
Nama Batuan : Serpih
Berat contoh mula – mula + wadah : 102
gram
Berat wadah
:
2
gram
Berat contoh
: 100
gram
Berat contoh setelah diayak
: 99,9992
gram
Berat contoh yang hilang
:
gram
0,0008
Interval Kelas
Titik Tengah Kelas "m"
Berat "f" (gram)
f(m)
(m-x)
f(m-x)2
f(m-x)3
f(m-x)4
Persen
Kumulatif Persen
-2.75 ke -2.25 -2.25 ke -1.75 -1.75 ke -1.25 -1.25 ke -0.75 -0.75 ke -0.25 -0.25 ke 0.25 0.25 ke 0.75 0.75 ke 1.25 1.25 ke 1.75 1.75 ke 2.25 2.25 ke 2.75 2.75 ke 3.25 3.25 ke 3.75 3.75 ke 4.25 4.25 ke 4.75
-2.5 -2 -1.5 -1 -0.5 0 0.5 1 1.5 2 2.5 3 3.5 4 4.5
0 0 0 0 0 0 17.2448 15.8691 14.4454 12.9766 16.0737 0 5.9812 8.865 8.5434 99.9992
0 0 0 0 0 0 8.6224 15.8691 21.6681 25.9532 40.18425 0 20.9342 35.46 38.4453 207.13655
0 0 0 0 0 0 -1.57138207 -1.07138207 -0.57138207 -0.07138207 0.42861793 0.92861793 1.42861793 1.92861793 2.42861793 3.85756136
0 0 0 0 0 0 42.5815778 18.2154979 4.71609766 0.06612097 2.95295294 0 12.2073253 32.9739625 50.3905541 164.104089
0 0 0 0 0 0 -66.9119279 -19.5157578 -2.69469365 -0.00471985 1.26568857 0 17.4396038 63.5941752 122.379403 115.551772
0 0 0 0 0 0 105.144204 20.908833 1.53969964 0.00033691 0.54249681 0 24.9145306 122.648867 297.212813 572.91178
0 0 0 0 0 0 17.244938 15.869227 14.4455156 12.9767038 16.0738286 0 5.98124785 8.86507092 8.54346835 100
0 0 0 0 0 0 17.244938 33.11416495 47.55968052 60.53638433 76.61021292 76.61021292 82.59146077 91.45653169 100
Mean (x)
= 2.071382071
Standard Deviation
= 1.281036307
Skewness
= 0.549662067
Kurtosis
= 2.127381961
Mean Cubed Deviation = 1.15552696 20 17.2448 15.8691 14.4454
18 16
12.9766
12 10
8.8658.5434
8
5.9812
6
Interval Kelas
butir menghalus
4.25 ke 4.75
3.75 ke 4.25
-0.25 ke 0.25
3.25 ke 3.75
-0.75 ke -0.25
0 2.75 ke 3.25
0 2.25 ke 2.75
0
1.75 ke 2.25
0
1.25 ke 1.75
0
0.75 ke 1.25
0
0.25 ke 0.75
0
-1.25 ke -0.75
0
-1.75 ke -1.25
2
-2.25 ke -1.75
4
-2.75 ke -2.25
Berat (gram)
14
16.0737
Metode Visher(1969)
Lampiran C-2 Analisis Granulometri No. Conto
: E – 02.160
Satuan Batuan : Batulanau–Serpih
Lokasi
: Pit E
Nama Batuan : Batulanau
Berat contoh mula – mula + wadah : 102
gram
Berat wadah
:
2
gram
Berat contoh
: 100
gram
Berat contoh setelah diayak
: 99,9993
gram
Berat contoh yang hilang
:
gram
0,0007
Interval Kelas
Titik Tengah Kelas "m"
Berat "f" (gram)
f(m)
(m-x)
f(m-x)2
f(m-x)3
f(m-x)4
Persen
Kumulatif Persen
-2.75 ke -2.25 -2.25 ke -1.75 -1.75 ke -1.25 -1.25 ke -0.75 -0.75 ke -0.25 -0.25 ke 0.25 0.25 ke 0.75 0.75 ke 1.25 1.25 ke 1.75 1.75 ke 2.25 2.25 ke 2.75 2.75 ke 3.25 3.25 ke 3.75 3.75 ke 4.25 4.25 ke 4.75
-2.5 -2 -1.5 -1 -0.5 0 0.5 1 1.5 2 2.5 3 3.5 4 4.5
0 0 0 0 0.1501 0 13.2493 17.6168 14.4934 12.1912 16.5009 0 6.6286 4.446 14.723 99.9993
0 0 0 0 -0.07505 0 6.62465 17.6168 21.7401 24.3824 41.25225 0 23.2001 17.784 66.2535 218.77875
0 0 0 0 -2.68780282 0 -1.68780282 -1.18780282 -0.68780282 -0.18780282 0.31219719 0 1.31219719 1.81219719 2.31219719 -0.69022533
0 0 0 0 1.08436502 0 37.742994 24.855112 6.85643205 0.42998237 1.60829458 0 11.4135308 14.6009247 78.7129245 177.30456
0 0 0 0 -2.91455936 0 -63.7027315 -29.522972 -4.71587326 -0.0807519 0.50210504 0 14.976803 26.4597546 181.999802 123.001577
0 0 0 0 7.83376086 0 107.517649 35.0674692 3.24359091 0.01516543 0.15675578 0 19.6525188 47.9502929 420.819431 642.256634
0 0 0 0 0.15010105 0 13.2493927 17.6169233 14.4935015 12.1912853 16.5010155 0 6.6286464 4.44603112 14.7231031 100
0 0 0 0 0.15010105 0.15010105 13.3994938 31.01641711 45.50991857 57.70120391 74.20221941 74.20221941 80.83086582 85.27689694 100
Mean (x)
= 2.187802815
Standard Deviation
= 1.331562245
Skewness
= 0.520989898
Kurtosis
= 2.042987685
Mean Cubed Deviation = 1.230024381 20
17.6169
18
16.5010
16 13.2494
14
12.1913
12 10 8
6.6286
6
4.4460
0
0
0
0
0.1501
0
-1.75 ke -1.25
-1.25 ke -0.75
-0.75 ke -0.25
-0.25 ke 0.25
2
-2.25 ke -1.75
4
-2.75 ke -2.25
0
Interval Kelas
butir menghalus
4.25 ke 4.75
3.75 ke 4.25
3.25 ke 3.75
2.75 ke 3.25
2.25 ke 2.75
1.75 ke 2.25
1.25 ke 1.75
0.75 ke 1.25
0 0.25 ke 0.75
Berat (gram)
14.7231
14.4935
Metode Visher (1969)
Kolom Litologi Bagian Barat KETERANGAN Satuan Batuan
Kolom Litologi Bagian Timur
Simbol Litologi
= Satuan Batulanau - Serpih
= batulanau
= Satuan Batubara
= serpih
= Satuan Batugamping
= batubara
= Satuan Batulempung
= breksi
= Satuan Batupasir Breksian
= batugamping
= Satuan Tanah Purba
Batas Satuan = batas tegas
= batupasir = batulanau = tufa
= batas erosional = moluska gastropoda
= interval studi khusus
UTARA
UTM UPS = 9905200 N - 9905300 N 763250 E - 763500 E
Sesar?
Ditambang
5 meter
Skala horizontal: 1 : 24500
UTM UPS = 9905950 N - 9906375 N 761325 E - 761750 E
Lampiran D-1 Korelasi Penampang Stratigrafi
= lintasan pengukuran penampang stratigrafi (PPS)
Kolom Litologi Bagian Timur INTERPRETASI STRATIGRAFI SIKUEN
KOLOM LITOLOGI
Kolom Litologi Bagian Barat
Early TST
SB
HST TST
27 SB
HST TST
INTERPRETASI STRATIGRAFI SIKUEN
KOLOM LITOLOGI
HST
Early TST
23
25
SB
HST
SB
Early TST
em - 5
24 SB
Early HST
HST
TST
KETERANGAN
HST
4 TST
26 SB
am-18
22
SB
Simbol Litologi
23
Early TST
SB
Early HST Early TST
SB
22
= serpih
em - 4 TST TST
21
21
= batulempung
SB
3 TST
SB
20 SB
TST
18
TST
Late HST Early TST
17
TST
3
SB
HST Early TST
19
18
= batugamping
SB 16
SB
HST
17
HST 15 Early TST
= batulanau
SB
SB
TST
SB
= moluska utuh dewasa
SB
am-17
HST
HST
16
= moluska utuh juvenil
am-16 TST
TST
14
SB
am-15 Early TST HST Early TST
SB
= moluska pecah - pecah
2 13
15
HST
SB
em - 1
Early HST 12 Early TST
TST
SB
Early HST
SB
TST
= lokasi pengambilan sampel
14 SB
HST
2 Early HST
11
Late TST
13
SB
Early TST
Late TST
HST Early TST
Early TST
Early TST
12
11 SB 10
HST
SB
= Batas tegas
SB
Late TST
10
Late TST
Early TST
TST
am-14
6
1
9 SB
Late TST
Early TST
5
Early TST Late TST Early TST
am-13 am-12 SB
em - 3
8 SB 7 SB
4
Simbol Sikuen Stratigrafi
Late TST
1
HST Early TST
= Batas erosional
SB
TST
SB
HST
Batas Satuan
SB
am-11
6 Early TST
SB
= Sequence Boundary/batas sikuen
SB
HST am-10
Early HST 3
HST
am-9
5 Early TST Early HST Early TST
2 SB
HST TST
= HST
TST
SB
em - 2
0
Early TST
am-8 am-7 am-6
1 SB
em - 1
meter
= TST
SB
HST
am-5
4
= siklus
am-4 TST
HST
am-3
Skala horizontal: 1 : 18750
0
meter
TST
SB
3
Catatan: - jarak dari kolom penampang sebelah barat ke sebelah timur sekitar 2,25 km - siklus kolom litologi bagian timur dicantumkan hanya hingga siklus ke-27 karena pengkorelasian hanya dapat dilakukan hingga siklus ke-23
Lampiran D-2 Korelasi Penampang Stratigrafi
TST Early TST
