Results 81 to 90 of about 802 (132)
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Tanah-tanah Dari Batuan Ultrabasik di Sulawesi: Kandungan Logam Berat dan Arahan Pengelolaan untuk Pertanian

Jurnal Tanah dan Iklim, 2020
Abstrak .  Pemetaan tanah semidetail skala 1:50.000 mengidentifikasi sekurangnya 1.628.485 ha lahan di Sulawesi tanahnya berkembang dari batuan ultrabasik.
Erna Suryani, Sofyan Ritung
semanticscholar   +1 more source

KORELASI ENDAPAN NIKEL LATERIT BERDASARKAN DATA GEOKIMIA DAN PETROGRAFI DI BLOK X PT. Z KABUPATEN MOROWALI UTARA PROVINSI SULAWESI TENGAH

Jurnal Teknik | Majalah Ilmiah Fakultas Teknik UNPAK
Daerah penelitian masuk ke dalam kompleks batuan ultramafik yang merupakan lokasi potensial terbentuknya endapan nikel laterit. Profil laterit di daerah penelitian terbagi menjadi empat zona, yaitu top soil, limonit, saprolit, dan bedrock.
Naurah MA'AAYISYA, MUHAMMAD AGUS KARMADI, & IIT ADHITIA
semanticscholar   +1 more source

KARAKTERISTIK FISIK, GEOKIMIA DAN SEBARAN ENDAPAN NIKEL LATERIT DAERAH LOJI BEACH, PULAU OBI, KABUPATEN HALMAHERA SELATAN, PROVINSI MALUKU UTARA

Buletin sumber daya geologi
Indonesia merupakan salah satu negara penghasil nikel terbesar di dunia. Salah satu daerah penghasil nikel di Indonesia berada di daerah Loji Beach yang menjadi daerah penelitian.
Eliana Trisusanti   +3 more
semanticscholar   +1 more source

Asosiasi Skandium dan Potensi Keberadaan Unsur Tanah Jarang pada Profil Laterit Nikel pada Daerah Wasile, Halmahera Timur, Maluku Utara

Jurnal Geologi dan Sumberdaya Mineral
Abstrak-Skandium dan Unsur Tanah Jarang merupakan sumber daya strategis yang berharga untuk berbagai aplikasi industri sehingga menjadi perhatian untuk eksplorasi sumber daya, ekstraksi berkelanjutan, dan aplikasi pada pengembangan teknologi.
Aditya Fadhlurrohman Putrananda   +2 more
semanticscholar   +1 more source

Alpine-type Serpentinites from the Auckland province—I. The Wairere Serpentinite

Journal of the Royal Society of New Zealand, 1973
Abstract The Wairere Serpentinite, exposed over 650 m along the trace of the Waipa Fault near Piopio, lies close to the boundary of the marginal and shelf facies of the New Zealand Geosyncline and hence close to Hatherton and Sibson's magnetic junction anomaly.
J. P. O'Brien, K. A. Rodgers
openaire   +1 more source

Alpine-type serpentinites from the Auckland Province—II. North Auckland serpentinites

Journal of the Royal Society of New Zealand, 1973
Abstract Eighty discrete lopolithic-shaped bodies of serpentinite ranging from 350 m3 to 24 000 m8 in size are found in North Auckland, south of Whangarei and east of Hatherton and Sibson's (1970) junction anomaly, within the Onerahi Chaos-breccia Formation. The bodies are confined to valley floors or low on the flanks of hills.
J. P. O'Brien, K. A. Rodgers
openaire   +1 more source

Serpentinite: What, Why, Where?

Elements, 2013
Rock-forming serpentine minerals form flat, cylindrical, and corrugated crystal microstructures, which reflect energetically efficient layering of alternate tetrahedral and octahedral sheets. Serpentinization of peridotite involves internal buffering of the pore fluid, reduction of oxygen fugacity, and partial oxidation of Fe 2+ to Fe 3+ .
B. W. Evans, K. Hattori, A. Baronnet
openaire   +1 more source

The Sierra Nevada serpentinites: the serpentinites most used in Spanish heritage buildings

Geological Society, London, Special Publications, 2014
Abstract Serpentinites from Sierra Nevada (Granada, south of Spain) have traditionally been used as ornamental elements in historical buildings, both indoors and outdoors. The cathedral, the Palace of Charles V, the Royal Chancellery in Granada and some others are good examples of their use.
Rafael Navarro   +3 more
openaire   +1 more source

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