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  1. 2301

    Mineral Lempung Hasil Ubahan Batuan Volkanik di Kuala Kurun Kabupaten Gunung Mas Kalimantan Tengah by Tjojudo, Suharto

    Published 1988
    “…Dibawah pengamatan mikroskop batu lempung ini terlihat mempunyai tekstur porfiritik sisa. Kaolinit berasal dari ubahan hldrotermal plagioklas, sedangkan hematit berasal dari ubahan plroksen dan mineral kedap cahaya lainnya. …”
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  2. 2302

    Adsorção de Cloreto e Potássio em Solos Tropicais. by Leandro Victor dos Santos, Helena Polivanov, Renata de Carvalho Jimenez Alamino, Vitor Hugo Gomes da Silva

    Published 2006-11-01
    “…It can be concluded that in most KCl solutions, the kaolinitic material adsorbed a higher amount of potassium than the lateritic soil. …”
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    Article
  3. 2303

    Suitability of Blending Rice Husk Ash and Calcined Clay for the Production of Self-Compacting Concrete: A Review by Abubakar Muhammad, Karl-Christian Thienel, Ricarda Sposito

    Published 2021-10-01
    “…Pozzolanic materials, like rice husk ash or calcined highly kaolinitic clays, have gained increased attention as supplementary cementitious materials in self-compacting concrete production. …”
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    Article
  4. 2304

    Geologi dan Persebaran Mineralisasi Timah, Unsur Radioaktif dan Unsur Tanah Jarang di Blok Lembah Jambu, Kecamatan Tempilang, Kabupaten Bangka Barat, Provinsi Kepulauan Bangka Beli... by Firdausi, Jalu Bias, Ali, Miftah Mukifin, Sutanto, Sutanto, Suprapto, Suprapto

    Published 2018
    “…Berdasarkan himpunan mineral yang ditemukan di lapangan dan analisa ASD, terdapat 5 zona alterasi yaitu Turmalin + Klorit, Turmalin + Kaolinit ± Phengit, Kaolinit + Kuarsa ± Illit ± Muskovit, Kaolinit ± Phengit ± Kuarsa dan Kuarsa + Kaolinit ± Palygorskit. …”
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    Article
  5. 2305

    Geologi dan Persebaran Mineralisasi Timah, Unsur Radioaktif dan Unsur Tanah Jarang di Blok Lembah Jambu, Kecamatan Tempilang, Kabupaten Bangka Barat, Provinsi Kepulauan Bangka Beli... by Firdausi, Jalu Bias, Ali, Miftah Mukifin, Sutanto, Sutanto, Suprapto, Suprapto

    Published 2018
    “…Berdasarkan himpunan mineral yang ditemukan di lapangan dan analisa ASD, terdapat 5 zona alterasi yaitu Turmalin + Klorit, Turmalin + Kaolinit ± Phengit, Kaolinit + Kuarsa ± Illit ± Muskovit, Kaolinit ± Phengit ± Kuarsa dan Kuarsa + Kaolinit ± Palygorskit. …”
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    Article
  6. 2306

    GEOLOGI DAN PERSEBARAN MINERALISASI TIMAH, UNSUR RADIOAKTIF DAN UNSUR TANAH JARANG DI BLOK LEMBAH JAMBU, KECAMATAN TEMPILANG, KABUPATEN BANGKA BARAT, PROVINSI KEPULAUAN BANGKA B... by Firdausi, Jalu Bias, Mukifin Ali, Miftah, Sutanto, Sutanto, Suprapto, Suprapto

    Published 2018
    “…Berdasarkan himpunan mineral yang ditemukan di lapangan dan analisa ASD, terdapat 5 zona alterasi yaitu Turmalin + Klorit, Turmalin + Kaolinit ± Phengit, Kaolinit + Kuarsa ± Illit ± Muskovit, Kaolinit ± Phengit ± Kuarsa dan Kuarsa + Kaolinit ± Palygorskit. …”
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    Conference or Workshop Item
  7. 2307

    GEOLOGI DAN PERSEBARAN MINERALISASI TIMAH, UNSUR RADIOAKTIF DAN UNSUR TANAH JARANG DI BLOK LEMBAH JAMBU, KECAMATAN TEMPILANG, KABUPATEN BANGKA BARAT, PROVINSI KEPULAUAN BANGKA B... by Firdausi1, Jalu Bias, Mukifin Ali, Miftah, Sutanto, Sutanto, Suprapto, Suprapto

    Published 2018
    “…Berdasarkan himpunan mineral yang ditemukan di lapangan dan analisa ASD, terdapat 5 zona alterasi yaitu Turmalin + Klorit, Turmalin + Kaolinit ± Phengit, Kaolinit + Kuarsa ± Illit ± Muskovit, Kaolinit ± Phengit ± Kuarsa dan Kuarsa + Kaolinit ± Palygorskit. …”
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  8. 2308

    STUDI ALTERASI HIDROTERMAL BAWAH PERMUKAAN LAPANGAN PANAS BUMI “BETA”, AMBON DENGAN METODE XRAY DIFFRACTION (XRD) by I.W.A. Sari, I.W.A. Sari, C.P.K.Vandani, C.P.K.Vandani, E. Mulyaningsih, E. Mulyaningsih, I. W. Warmada, I. W. Warmada, P. Utami, P. Utami, Y. Yunis, Y. Yunis

    Published 2014
    “…Keterdapatan haloisit, kaolinit dan sulfur yang berasosiasi dengan pirit, anhidrit dan kuarsa pada kedalaman <260 m mengindikasikan adanya fluida asam. …”
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    Article
  9. 2309

    Ethylene Adsorption on Acid-Treated Clay Minerals by Burcu Erdoğan Alver, Meryem Sakızcı

    Published 2012-03-01
    “…The adsorption of ethylene (C 2 H 4 ) on five clay minerals (sepiolite, two kaolinites and two bentonites) and on forms treated with 1 M HCl solution (SH, K1H, K2H, B1H and B2H) was investigated. …”
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    Article
  10. 2310

    ÜZÜMDERE FORMASYONU (AKSEKİ KUZEYBATISI, ANTALYA) KUMTAŞLARININ MlKRODOKUSAL ÖZELLİKLERİ by Turhan AYYILDIZ, Erdoğan TEKİN, Nurettin SONEL, Mehmet BÜLBÜL

    Published 1995-10-01
    “…demiroksit, klorit ve kaolinit olduğu tespit edilmiştir Aynca kalsit ve demiroksit çimento, çatlaklan dolduran ikincil boşluk dolgusu şeklinde gelişmiştir Otijenik kil oluşumlan ve kuvarslarda çevresel büyümelerin gözlendiği birimde, gözeneklimin yok denecek Kadar az olduğu saptanmıştır.…”
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    Article
  11. 2311

    Depositional model of the Ipixuna Formation (Late Cretaceous-?Early Tertiary), Rio Capim area, northern Brazil by Antônio Emídio de Araújo Santos Jr., Dilce de Fátima Rossetti

    Published 2021-03-01
    “…The lower part of this unit emphasized herein, known as the "soft kaolin", consists mostly of kaolinitized sandstones and mudstones with well preserved sedimentary structures that are particularly favorable for facies analysis and paleoenvironmental reconstructions. …”
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    Article
  12. 2312

    An assessment of phosphorus soil tests for some tropical acid soils in Southern Thailand by Nilnond, C., Leowarin, W., Maneepong, S.

    Published 2005-03-01
    “…Pot experiment was conducted in five acid soils [Bangnara (Ba): Clayey, kaolinitic, Typic Paleaquults; Ao Luk (Ak): Clayey, kaolinitic, Rodic Paleudults; Na Thon (Ntn): Clayey, mixed, Typic Tropudults; Phuket (Pk): Clayey, kaolinitic, Typic Paleudults; Kohong (Kh): Coarse-loamy,siliceous, Typic Paleudults] which have different parent materials using completely randomized design with 3 replications. …”
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  13. 2313

    Geologi, Alterasi Hidrotermal dan Mineralisasi Bijih Endapan Emas Epitermal Sulfidasi Tinggi Pit Ramba Joring, Desa Aek Pining, Kecamatan Batangtoru, Kabupaten Tapanuli Selatan, Pr... by Manurung, Sylvia Y., Idrus, Arifudin, Pulungan, Benny A. A.

    Published 2019
    “…Tipe alterasi yang berkembang terdiri dari zona argilik (ilit-smektit+kaolinit+ilit), argilik lanjut (silika+dikit+alunit+kaolinit) dan silika vuggy-masif. …”
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    Article
  14. 2314

    Depositional model of the Ipixuna Formation (Late Cretaceous-?Early Tertiary), Rio Capim area, northern Brazil by Antônio Emídio de Araújo Santos Jr., Dilce de Fátima Rossetti

    Published 2021-03-01
    “…The lower part of this unit emphasized herein, known as the "soft kaolin", consists mostly of kaolinitized sandstones and mudstones with well preserved sedimentary structures that are particularly favorable for facies analysis and paleoenvironmental reconstructions. …”
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    Article
  15. 2315

    Depositional model of the Ipixuna Formation (Late Cretaceous-?Early Tertiary), Rio Capim area, northern Brazil by Antônio Emídio de Araújo Santos Jr., Dilce de Fátima Rossetti

    “…The lower part of this unit emphasized herein, known as the "soft kaolin", consists mostly of kaolinitized sandstones and mudstones with well preserved sedimentary structures that are particularly favorable for facies analysis and paleoenvironmental reconstructions. …”
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    Article
  16. 2316

    Effects of rainfall intensity and slope gradient on soil sealing and crusting, erosion, and phosphorus solubilizing bacteria by Kaya Mrubata, Adornis D. Nciizah, Isaiah I.C. Wakindiki, Fhatuwani N. Mudau

    Published 2024-03-01
    “…The smectitic soils formed the strongest crusts with S2 exhibiting significantly (p < 0.05) higher crust strength (18.54 Kpa) at an intensity of 45 mm/h and slope of 8° On the other hand, soil K3 (kaolinitic) had the lowest crust strength (5.4 Kpa) at an intensity of 100 mm/h and slope of 8° Soil loss increased with higher rainfall intensity and steeper slopes for the kaolinitic soils with K1 being most erodible (468.2 kg/ha) at an intensity of 100 mm/h and slope of 8° The number of phosphate solubilising bacteria decreased with increasing rainfall intensity. …”
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    Article
  17. 2317

    THE EFFECT OF THE POZZOLANIC ACTIVITY OF DIFFERENT MICRO-FILLERS ON PORTLAND CEMENT HYDRATION by Rimvydas Kaminskas, Irmantas Barauskas, Kubiliute Raimonda, Monstvilaite Deimante

    Published 2020-03-01
    “…All investigated pozzolanic active micro-fillers promote the formation of the calcium silicate hydrates, however, only in the samples with the most active (kaolinitic clay) micro-filler after 28 days of hardening clearly identifies the pozzolanic reaction. …”
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    Article
  18. 2318

    Effect of the Introduction of Reactive Fillers and Metakaolin in Waste Clay-Based Materials for Geopolymerization Processes by Caterina Sgarlata, Alessandra Formia, Francesco Ferrari, Cristina Leonelli

    Published 2021-03-01
    “…Three kinds of clayey wastes from mining operations—halloysitic, kaolinitic and smectitic clays—were tested as potential precursor of geopolymeric materials in view of a potential valorisation of these by-products. …”
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    Article
  19. 2319

    TEKKE VOLKANİTLERİNDE HİDROTERMAL ALTERASYON ÜRÜNÜ KİL MİNERALLEŞMELERİ ( ÇUBUK, ANKARA KD) by Asuman BESBELLİ, Baki VAROL

    Published 2002-06-01
    “…Bunların zonlanması ise içten dışa doğru kaolinit, montrollonit ve illit şeklinde gelişmiştir. …”
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  20. 2320

    Effect of compaction on microbial activity and carbon and nitrogen transformations in two oxisols with different mineralogy by Sérgio Ricardo Silva, Ivo Ribeiro da Silva, Nairam Félix de Barros, Eduardo de Sá Mendonça

    Published 2011-08-01
    “…Therefore, it is possible to conclude that under controlled conditions, the oxidic-gibbsitic Oxisol (LVA) was more susceptible to the effects of high compaction than the kaolinitic (LA) as far as organic matter cycling is concerned; and compaction pressures above 540 kPa reduced the total and organic nitrogen in the kaolinitic soil (LA), which was attributed to gaseous N losses.…”
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