106 research outputs found
Corpus de Dislocations à droite en anglais
No full textA corpus of right dislocations made up of sentences taken from literature and read by six English-speaking people (men and women), plus a few examples taken from movies (126 recordings in total).Corpus de dislocations à droite en anglais composé de 20 phrases tirées de textes littéraires lues par six anglophones (hommes et femmes), ainsi que quelques exemples tirés de films, soit au total 1997 mots (126 enregistrements).LEONARDUZZI, Laetitia, HERRY, Nadine (2006). Les dislocations à droite : entre détachement et intégration. Quelques aspects syntaxiques et prosodiques. Actes du Colloque de l'ALOES, mars 2006 (13 pages).http://lpl-aix.fr/article/4457LEONARDUZZI, Laetitia; HERRY, Nadine (2006). Les dislocations à droite : entre détachement et intégration. Quelques aspects syntaxiques et prosodiques.http://lpl-aix.fr/article/445
PENGARUH LINGKUNGAN PENGENDAPAN TERHADAP KUALITAS BATUBARA DAERAH BINDERANG, LOKPAIKAT,TAPIN, KALIMANTAN SELATAN
No full textDaerah penelitian masuk dalam konsesi wilayah penambangan batubara PT. Kalimantan Prima Persada. Secara administratif berada di Desa Binderang Kecamatan Lokpaikat Kabupaten Tapin Propinsi Kalimantan Selatan. Dan secara geografis terletak pada 303500 mE – 304500 mE dan 9673700 mN – 9676300 mN. Penelitian ini bertujuan untuk mengetahui aspek lingkungan pengendapan yang menyebabkan terjadinya perbedaan kualitas berdasarkan pada kadar abu, kandungan sulfur dan nilai kalori pada lapisan batubara daerah telitian.Daerah telitian secara geomorfologi termasuk dalam satuan bentuk lahan struktural dengan pola pengaliran dendritik. Stratigrafi merupakan Cekungan Barito dari Formasi Warukin Atas sebagai Formasi pembawa batubara yang brumur Miosen Tengah. Litologi terdiri atas Satuan Batulempung yang disusun oleh perselingan batupasir dan batulempung dengan sisipan batulanau, serpih dan batubara. Lingkungan pengendapan pada transitional lower delta plain, dengan sub-lingkungan terdiri dari marsh, levee-splay, creavasse-splay dan channel-fill. Pengamatan langsung di lapangan, setiap lokasi pengamatan lapisan batuan dan batubara dalam keadaan tidak lapuk. Batubara dengan ciri-ciri fisik berwarna hitam gelap, kilap kusam, relatif berat, parting berupa lempung karbonan. Lapisan batubara kontak dengan lapisan batupasir dan batulempung.Parameter kualitas yang digunakan adalah kadar abu, kandungan sulfur dan nilai kalori. Dari hasil analisa proksimat, batubara daerah telitian menunjukan kadar abu berkisar 1,7% adb – 14,5% adb, kandungan sulfur berkisar 0,09% adb – 0,2%adb, dan nilai kalori 5105 kcal/kg – 6023 kcal/kg. Kualitas batubara daerah telitian dipengaruhi oleh lingkungan pengendapan beserta genesa yang menyertai pembentukan batubara
Dendrogram
No full textDendrogram of a hydrochemical cluster generated by hierarchical
cluster analysis
Geologi dan Pengaruh Struktur Kekar Terhadap Kestabilan Lereng Desain Pit Pada Tambang Terbuka Batubara Kecamatan Lawang Kidul, Kabupaten Muaraenim, Sumatra Selatan
Get PDFOpen pit mining system is one of the systems used to exploitation coal resources by stripping the overburden to produce slopes. Unstable slopes will result in landslides. Fractures are one of the causes of landslides. The purpose of the study was to determine the geological and geotechnical conditions of the area to create an optimal and safe slope design. The research area is administratively located in Tanjung Lalang, Lawang Kidul District, Muara Enim Regency, South Sumatra Province, which is a mining business permit (IUP) area of PT Bukit Asam Tbk. Geographically located at the geographical coordinates 103° 49\u270 "BT - 103° 50\u2720" BT and 3° 50\u2759" LS - 3° 50\u279" LS. The research methods used are literature studies, geological mapping, profiles, Scanlines, data analysis, rock mass rating, RQD, RMR, SMR, GSI, kinematic analysis, and quantitative analysis to determine the FK (Safety Factor) value. The research area is included in the South Sumatra basin which is included in the Muara Enim Formation which consist of Muara Enim mudstone units aged Middle - Late Miocene, and Alluvial units aged Holocene in the form of loose material accumulation. The geological structure that developed in the research area is a left slip fault with SE-NW emphasis and fractures that have NE-SW direction emphasis. At observation location 7 has an RQD value of 22.2543%, RMR 48.4210, SMR 46.81, GSI 40.8654, at observation location 10 has an RQD value of 35.1343%, RMR 52.642 8, SMR 49.17, GSI 48.2671, at observation location 24 has an RQD value of 57.2979, RMR 64.375, SMR 61.27 and GSI 60.836 at observation location 2 has a GSI value of 30 and at observation location 16 has a GSI value of 25. Based on the results of the analysis of the FK value without the influence of fractures on Section A-A\u27 2.364, section B-B\u27 1.889 and section C-C\u27 2.546, the FK value with fractures on section A-A\u27 2.326, section B-B\u27 1.172 and section C-C\u27 1.389 based on the results of linear analysis of the influence of fractures on the decrease in FK value has a determination value of R² = 0.5836 (moderate) and the effect of the number of fractures on the decrease in FK value has a determination value of R² = 0.6948 (Strong). Based on the results of kinematic analysis on sections A-A\u27 and C-C\u27 have a Wedge Landslide Potential type while on section B-B\u27 has a Toppling landslide potential type. Recommendations for increasing slope stability at LP 7 by changing the slope direction N 288ºE and slope 55º, at LP 10 slope direction N 325ºE and slope 62º, LP 24 slope direction N 005ºE and slope 44º. Positive geological potential in the research area is in the form of economical coal mines and PLTU, negative geological potential in the research area is in the form of landslides, acid mine water, air pollution and bare forests
Piezometric Map
No full text(A) Piezometric map with
the groundwater flow (®) in
fault compartment. (B) Piezometric variogram level with directional of (---)
experimental and (-·-·-) modeled
BATIK KONTUR DESA WISATA KALIBIRU
Get PDFKalibiru Tourism Village develops eco-tourism potential by prioritizing aspects of nature conservation, socio-cultural-economic empowerment of local communities, and learning and education. Now, tourist visits have decreased since 2018 and are increasingly critical during the COVID-19 pandemic. So, residents are trying to explore the potential for creative tourism in the village in the form of the Kalibiru Kontur Batik, which expects to support the residents\u27 economy by developing batik that symbolizes village identity through motifs and has a philosophy as a form of local wisdom.The Kalibiru Contour Batik is a manifestation of the results of geological studies harmonized with the state of the landscape in the Kalibiru Tourism Village in the form of hills, valleys, and rivers reflected in the form of contours contained in Topographic Maps and Geological Maps. The contour on the topographic map are the motifs of the Kalibiru Contour Batik, and the Legend on the Geological Map, which tells the village\u27s history, is the basis for the philosophy of the Kalibiru Contour Batik
Vf and Smf Map with variogram
No full text(A) River pattern flow
NW to SW direction, (B) Sinuosity of
mountain front (Smf) to determine the
class of tectonic activity level and valley ratio index (Vf) to determine the
uplift class. (C) Variogram of Smf and (D) variogram of Vf
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