Struktur Bawah Permukaan Intrusi Batuan Beku Di Parangtritis, Pantai Selatan Yogyakarta Ditinjau Dari Data Anomali Medan Gravitasi by Perpustakaan UGM, i-lib

“…Keyword : Bouguer anomaly, igneous rock intrusion, density, strike length…”

KELIMPAHAN UNSUR TANAH JARANG DI DALAM ALTERASI DAN MINERALISASI TIMAH PRIMER: STUDI KASUS DI BANGKA TENGAH by Ayunda, Friska Putri, Setijadji, Lucas Donny, Ferdila, Hendra, Murtono, Anton

“…REE abundance within various types of lithology and alteration/mineralisation can reach up to: 76.6 MORB in quartz monzonite, 125.53 MORB in leucogranite dike, 269.61 MORB in foliated quartz monzonite, 7.75 MORB in quartz+tourmaline vein from seritized quartz monzonite, 60.46 MORB in argilic alteration of igneous rock, 87.54 MORB in greisenised igneous rock, 71.13 MORB in metasandstone, 42.55 MORB in silisified meta-sandstone, and 33.74 MORB in seritized meta-sandstone. …”
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Indicating the Provenance of Recent Sediment in Yogyakarta Basin from Sediment Geochemistry: Preliminary Results by , D. H. Amijaya

“…The sedimentary material in the upstream area is originally comes from intermediate igneous rock of the volcanic range at north (especially Merapi Volcano), while products of rock weathering from Kulon Progo Mountain Range and Southern Mountain contribute the sedimentary<br /> material in the middle up to the downstream area</p>…”

GEOTAGE: GEOLOGICAL SHAREWARE APPLICATION FOR GEOLOGY OBJECT by Tara Shinta Dewi, at. al

“…Indonesia has complete geological objects such as outcrops (igneous rock, sedimentary rock, metamorphic rock and pyroclastic rock), mineral deposit, active and non-active volcano also geoheritage as Indonesia precious assets. …”
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IDENTIFIKASI DAERAH RAWAN GERAKAN TANAH DI KOTA LIWA, LAMPUNG BARAT MENGGUNAKAN METODE GEORADAR DAN GEOLISTRIK by , Yusraida Khairani, , Prof. Dr. Sismanto, M.Si

“…Liwa subsurface structure is arranged by quartenary sediment, clay (1- 100 ï��m), sand (8 â�� 4000 ï��m) and igneous rock, granit ( 5.000 â�� 1.000.000 ï��m) and from the results of the data analysis found that indication of a weak zone of the fault by line 1, 2, 3, 5, 6.…”

MODEL GEOLOGI DAN DESAIN PIT TAMBANG ENDAPAN NIKEL LATERIT PADA DAERAH WATUDEMBA, KECAMATAN PALANGGA, KABUPATEN KONAWE SELATAN PROVINSI SULAWESI TENGGARA by , LEDIYANTJE LINTJEWAS, , Dr.-rer.nat. Arifudin Idrus, ST., MT

“…Geological model at study area is dominated by sedimentary rocks of reef limestone laid unconformably above ultramafic igneous rocks. Ultramafic igneous rocks age was Cretaceous while reef limestone in Miocene age. …”

Magmatism and Porphyry Cu-Au Mineralisation at Randu Kuning Prospect Selogiri Area, Central Java by Sutarto, ., Idrus, Arifudin, Putranto, Sapto, Harijoko, Agung, Setidjaji, Lucas Donny, Meyer, Michael, Dany, Rama

“…The Randu Kuning area and its vicinity is a part of the East Java Southern Mountain Zone, mostly occupied by both plutonic and volcanic igneous rocks, volcaniclastic rocks, silisiclastic rocks and also carbonate rocks.…”
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PENGARUH KONDISI BATUAN TERHADAP KIMIA AIR TANAH DI DAERAH KOTA JAYAPURA DAN SEKITARNYA by , Bodian Davin Panggabean ST, , Dr. Doni Prakasa Eka Putra, ST., MT.

“…Based on the three lithological condition, it could be seen that TDS and Cl- content is greater on sedimentary rocks than in igneous rocks.…”

PEMODELAN TIGA DIMENSI (3D) STRUKTUR BAWAH PERMUKAAN BUMI DI PROVINSI PAPUA BARAT BERDASARKAN ANALISIS DATA GRAVITASI by , Richard Lewerissa, , Dr. Ing. Ari Setiawan

“…Included: limestone, especially coral limestone, conglomerate, sandstone, and clay was estimated from moicene to pleistocene and early holocene in Autralia plate, mid miocene to end Pliocene in Pasifik plate. Igneous rocks as lavas, basalt, and andesite especially in Arfak mountain from eocene to early miocene. …”

GIS Mineral Potential Mapping for Bauxite Deposits Using Analytical Hierarchy Process (AHP) Method in West Kalimantan, Indonesia by , YANG VIRINRATH, , Dr. Lucas Donny Setijadji

“…The highestprobability area occurs in the southeastern part of the study area, associated with large bauxite deposits produced by lateritization of Cretaceous igneous rocks within undulating hills morphology thatcan be treated as the most potential site for further exploration. …”