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Abstrak :
Analisis fisika batuan adalah salah satu komponen kunci dalam eksplorasi, pengembangan, dan produksi hidrokarbon yang menyediakan hubungan antara parameter reservoar geologi dan sifat seismik. Tujuan dari penelitian ini adalah untuk menganalisis bagaimana pengaruh kandungan mineral lempung terhadap respon seismik AVO pada reservoar batupasir berdasarkan persamaan Gassmann di pemodelan fisika batuan. Metode yang dilakukan dalam penelitian ini adalah pemodelan fisika batuan dari dua data sumur X-19 dan X-15 di Lapangan 'D', Formasi Balikpapan, Cekungan Kutai. Pemodelan yang dilakukan baik pada sumur X-15 dan X-19, hanya dilakukan pada dua zona perwakilan. Zona A dan C untuk sumur X-15 serta zona K dan Q untuk sumur X-19. Proses pemodelan fisika batuan terdiri dari pemodelan mineral, fluida, serta kerangka batuan. Ketiganya dengan persamaan Gassmann akan digunakan untuk menghitung nilai pemodelan Vp, Vs, dan rb. Impedansi akustik dan impedansi elastik kemudian dihitung untuk mendapatkan nilai R q dari pendekatan Zoeppritz, dengan menggunakan persamaan Shuey. Sebagai kesimpulan, penelitian ini menunjukkan bahwa pengaruh yang paling terlihat dalam pemodelan adalah pada sumur X-19 di zona Q unsur mineral lempung adalah Smectite dan sumur X-15 di zona C unsur mineral lempung adalah Illite. Baik zona Q dan C terindikasi tersaturasi oleh gas. Smectite yang memiliki nilai modulus onggok dan rigiditas paling rendah diantara tipe lempung lainnya, mampu memperlambat kecepatan yang menjalar pada zona Q. Illlite yang memiliki nilai modulus onggok dan rigiditas yang lebih tinggi bila dibandingkan dengan Kuarsa, mampu mempercepat kecepatan yang menjalar pada zona A. Dan untuk nilai rb pemodelan di kedua zona Q dan C, menjadi lebih kecil bila dibandingkan dengan data riil.

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Rock physics analysis is one of the key components in the exploration, development, and production of hydrocarbons that provide a link between geological reservoir parameters and seismic properties. The purpose of this study was to analyze the effect of clay mineral content on AVO seismic response on sandstone reservoir based on Gassmann equation in rock physics modeling. The method used in this research was rock physics modeling of two well data X 19 and X 15 in D Field, Balikpapan Formation, Kutai Basin. Modeling performed both on wells X 15 and X 19, was done on two representative zones. Zone A and C for well X 15 and zone K and Q for well X 19. The process of rock physics modeling consists of mineral, fluid, and modeling. All those three will be assembled with Gassmann equation to calculate the modeling of Vp, Vs, and rb. The acoustic impedance and shear impedance were then calculated to obtain the value of R q from Zoeppritz approximation, using the Shuey equation. The most visible influence showed in modeling on well X 19, zone Q clay mineral element is Smectite and well X 15 in zone C clay mineral element is Illite. Both zone Q and C were indicated saturated by gas. Smectite which has the lowest bulk modulus and rigidity value of the other clay type, capable of slowing the velocity on zone Q. Illlite which has bulk modulus and rigidity value compared by Quartz, able to accelerate the velocity that propagates in zone A. And the value of rb modeling in both zones Q and C, becomes smaller when compared with real data.

Abstrak :
[ABSTRAK
Aplikasi atribut seismik 3D dan sifat fisik batuan telah dapat memodelkan reservoar A Formasi Ledok Lapangan X Blok Cepu. Beberapa atribut seismik yang sesuai untuk mengidentifikasi penyebaran reservoar dilapangan ini adalah root mean square (rms), sweetness, dan impedansi akustik relatif. Dimana ketiga atribut seismik tersebut memperlihatkan suatu anomali amplitudo berupa bright spot yang diidentifikasi sebagai reservoar A dan memperlihatkan pola penyebaran berarah selatan-utara. Fasies reservoar A yang merupakan batugamping pasiran adalah reservoar yang sangat baik dalam menyimpan hidrokarbon gas dengan porositas 19% dan saturasi air sebesar 40%. Adanya faktor ketidakpastian dalam penentuan batas penyebaran reservoar A dari atribut seismik, model reservoar A di bagi menjadi tiga bagian yaitu perkiraan optimis (P90), perkiraan sedang (P50) dan perkiraan pesimis (P10). Keberadaan hidrokarbon gas di Lapangan X dikontrol oleh suatu perangkap stratigrafi bukan perangkap struktur hal ini terlihat dari tidak adanya tutupan (klosur). Berdasarkan sebaran reservoar melalui integrasi atribut seismik, properti batuan dan model reservoar diusulkan 4 (empat) sumur pemboran untuk mengembangkan lapangan gas X.

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ABTRACT
Application of 3D seismic attributes and physical properties of reservoir rocks have been to model the formation Ledok A Field X Cepu Block. The seismic attributes, which can be used to identify distribution of the reservoir in this field were the root mean square (rms), sweetness, and relative acoustic impedance. The attributes of the seismic amplitude anomaly shows a bright spot in the form identified as reservoars A and show the pattern of northsouth trending deployment. A reservoir facies which is a sandy limestone reservoir was very good at keeping a hydrocarbon gas with 19% porosity and water saturation of 40%. The existence of uncertainty in the determination of reservoir distribution limit of seismic attributes. A reservoir model was divided into three parts, optimistic estimate (P90), moderate estimate (P50) and pesimistic estimate (P10). The existence of hydrocarbon gases in field X in was control by a stratigraphic traps compared to traps structure as seen from the absence of cover (closur). Based on integration of seismic attributes, rock properties and reservoar model proposed four (4) wells drilling to develop the gas field X.;Application of 3D seismic attributes and physical properties of reservoir rocks have been to model the formation Ledok A Field X Cepu Block. The seismic attributes, which can be used to identify distribution of the reservoir in this field were the root mean square (rms), sweetness, and relative acoustic impedance. The attributes of the seismic amplitude anomaly shows a bright spot in the form identified as reservoars A and show the pattern of northsouth trending deployment. A reservoir facies which is a sandy limestone reservoir was very good at keeping a hydrocarbon gas with 19% porosity and water saturation of 40%. The existence of uncertainty in the determination of reservoir distribution limit of seismic attributes. A reservoir model was divided into three parts, optimistic estimate (P90), moderate estimate (P50) and pesimistic estimate (P10). The existence of hydrocarbon gases in field X in was control by a stratigraphic traps compared to traps structure as seen from the absence of cover (closur). Based on integration of seismic attributes, rock properties and reservoar model proposed four (4) wells drilling to develop the gas field X.;Application of 3D seismic attributes and physical properties of reservoir rocks have been to model the formation Ledok A Field X Cepu Block. The seismic attributes, which can be used to identify distribution of the reservoir in this field were the root mean square (rms), sweetness, and relative acoustic impedance. The attributes of the seismic amplitude anomaly shows a bright spot in the form identified as reservoars A and show the pattern of northsouth trending deployment. A reservoir facies which is a sandy limestone reservoir was very good at keeping a hydrocarbon gas with 19% porosity and water saturation of 40%. The existence of uncertainty in the determination of reservoir distribution limit of seismic attributes. A reservoir model was divided into three parts, optimistic estimate (P90), moderate estimate (P50) and pesimistic estimate (P10). The existence of hydrocarbon gases in field X in was control by a stratigraphic traps compared to traps structure as seen from the absence of cover (closur). Based on integration of seismic attributes, rock properties and reservoar model proposed four (4) wells drilling to develop the gas field X., Application of 3D seismic attributes and physical properties of reservoir rocks have been to model the formation Ledok A Field X Cepu Block. The seismic attributes, which can be used to identify distribution of the reservoir in this field were the root mean square (rms), sweetness, and relative acoustic impedance. The attributes of the seismic amplitude anomaly shows a bright spot in the form identified as reservoars A and show the pattern of northsouth trending deployment. A reservoir facies which is a sandy limestone reservoir was very good at keeping a hydrocarbon gas with 19% porosity and water saturation of 40%. The existence of uncertainty in the determination of reservoir distribution limit of seismic attributes. A reservoir model was divided into three parts, optimistic estimate (P90), moderate estimate (P50) and pesimistic estimate (P10). The existence of hydrocarbon gases in field X in was control by a stratigraphic traps compared to traps structure as seen from the absence of cover (closur). Based on integration of seismic attributes, rock properties and reservoar model proposed four (4) wells drilling to develop the gas field X.]

Abstrak :
ABSTRAK
Eksplorasi dan produksi minyak dan gas bumi migas di Indonesia sampai sekarang masih terfokus pada migas konvensional dibandingkan migas nonkonvensional seperti hidrokarbon serpih. Hidrokarbon serpih adalah salah satu sumber energi migas yang terdapat di batuan induk memiliki material organik yang kaya dan telah mencapai kematangan, pada kondisi dan tipe tertentu dapat berfungsi sebagai reservoar minyak dan gas. Formasi Talang Akar adalah batuan induk dari Cekungan Jawa Barat Utara, berpotensi sebagai sistem petroleum nonkonvensional. Pada penelitian ini diintegrasikan analisis geokimia batuan induk, sifat fisika batuan dan interpretasi seismik yang menjadi dasar untuk melihat hubungan kekayaan dan kematangan material organik serta pesebarannya sebagai potensi hidrokarbon serpih di Cekungan Jawa Barat Utara. Hasil analisis geokimia batuan induk pada Formasi Talang Akar didapat tingkat kekayaan materi organik berkisar antara 0.57 ndash;1.81 wt fair-good , jendela awal kematangan pada kedalaman 3200 m dan tipe kerogen II/III menghasilkan minyak dan gas. Analisis sifat fisik batuan meliputi perhitungan Vshale, porositas, saturasi dan perhitungan TOC secara kontinu menggunakan Metode Passey untuk mengetahui nilai TOC pada setiap kedalaman pada Formasi Talang Akar. Hasil analisis selanjutnya adalah melakukan interpretasi seismik dengan metode inversi impedansi akustik model based untuk melihat persebaran batuan serpih dengan nilai 32000 ndash;54000 ft/s g/cc, arah penyebaran batuan serpih sebagai potensi hidrokarbon serpih berada di barat dan barat laut daerah penelitian. Kata Kunci:. Eksplorasi dan Produksi Migas, Hidrokarbon Serpih, Material Organik, Formasi Talang Akar, Geokimia Batuan Induk, Sifat Fisika Batuan, Inversi Seismik Impedansi Akustik

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ABSTRACT
Shale Hydrocarbon Analysis Based on Geochemical and Seismic Data in Northwest Java BasinAbstract Hydrocarbon exploration and production in Indonesia until now still focused on conventional energy rather than unconventional energy, which is shale hydrocarbon. Shale hydrocarbon is one of energy which contained in source rock that has high organic richness and been reached, in specific condition could be reservoir rock. Talang Akar Formation is source rock of Northwest Java Sedimentary Basin. This research was conducted on the integration of the three methods including organic geochemical analysis, seismic interpretation and petrophysics which became the basis for the wealth of organic material see the relationship and maturity of organic material also the distribution on the potential of shale hydrocarbon in the region. The analysis of Organic Geochemistry in Talang Akar Formation obtained the level of wealth of organic matter ranged from 0.57 ndash 1.81 wt fair good , the initial maturity of the window at a depth of 3200 m and category II III kerogen type produces oil and gas. The analysis of petrophysics which include calculation of TOC based on Passey Method continuously, the results of the analysis of this petrophysics validated with the value of the laboratory analysis. The next step is doing seismic interpretation with acoustic impedance inversion method to see the spread of the shale rocks with a value 32000 ndash 54000 ft s g cc, the direction of spread of shale rocks as shale hydrocarbon potential in the West and Northwest areas of research area. Keyword Hydrocarbon exploration, unconventional energy, geochemical, shale hydrocarbon, Organic Geochemistry, Talang Akar Formation, Acoustic Impedance Seismic Inversion.