bluuebunny/crossref_metadata_2025_split huggingface dataset:
EKSISTENSI PROGRAM RADIO LOKAL THE RADIO FM PADA ERA REVOLUSI INDUSTRI 4.0 DI KOTA KENDARI
Authors: Amelia Marsya , Dilla Sumadi , Syahartijan Laode Muh. 
Published: September 2021

Revolusi industri 4.0 merupakan penggabungan antara teknologi otomatisasi dengan teknologi cyber. Oleh sebab itu teknologi dan internet menjadi tantangan bagi media konvensional seperti radio untuk tetap mempertahankan eksistensinya. Salah satu radio yang mengikuti perkembangan teknologi internet agar tetap eksisdi Kota Kendari adalah THE RADIO FM. Eksistensi The Radio FM dilihat dari program-program unggulannya yang menjadi alasan pendengar mau mendengarkan THE RADIO FM. Program Unggulannya memiliki konten yang menarik, kreatif dan inovatif serta informasi yang diberikan informasiup to date. Namun, Pengelolah THE RADIO FM sadar betul akan dampak revolusi industri 4.0 ini pada eksistensi radionya. Tujuan penelitian ini adalah untuk mengetahui apa saja eksistensi program radio lokal The Radio FM dalam menghadapi revolusi industri 4.0 di Kota Kendari. studi ini menggunakan metode penelitian kualitatif. Hasil penelitian ini menunjukkan bahwa untuk mempertahankan eksistensinya radio lokal The Radio FMharus memenuhi kebutuhan akan pendengarnya. Apabila kebutuhan pendengar terpenuhi maka radio tersebut bisa eksis. studi ini menggunakan teori normatif media oleh Denis McQuail. Penentuan Informan berjumlah enam orang yang dipilih dengan pertimbangan dan tujuan tertentu, hasil dari penelitian ini radio lokal The Radio FM telah memenuhi aspek-aspek penunjang eksistensinya yaitu memiliki program unggulan berupa Spageti, Sore DoReMi, dan MalaMalam dimana ketiganya memiliki konten yang menarik, kreatif dan inovatif serta informasi yang uptodate, yang bisa diakses oleh pendengar menggunakan tape radio, streaming dan handphone. untuk terus eksis media harus bertindak sesuai dengan kebutuhan masyarakat dalam memenuhi kebutuhan akan informasinya untuk itu disarankan untuk berhati-hati dalam memberikan informasi agar tidak menyinggung pendengar.Kata-kata Kunci: eksistensi radio ; revolusi industri 4.0; Teori Normatif
Accountability Studies in Religious Non-Profit Organizations: Possible Contextual and Application Gaps
Authors: Ali Zubaidah Mohd , Mahadi Rozaidy 
Published: September 2021

Having substantial accountability standards and practices is a vital practice to ensure the survival of Religious-Based Non-Profit Organisations (RNPOs). This is because the RNPOs are not only representing the religion’s ideals but at the same time, there are also responsible in disseminating ethical massage and good values in the community. Since the RNPOs played a significant role in society, many studies have highlighted the need to explore more accountability issues involving RNPOs. Hence, this study aims to provide a taxonomical review of literature that examined RNPOs’ accountability practices and subsequently, suggesting plausible contextual and application gaps for future research. In so doing, this study utilised van Helden and Nortcott’s (2010) and Rozaidy, Siti Nabiha, Rasid, and Raman (2017) taxonomical methods in categorising accountability studies in RNPOs. As a result, four main themes have been identified from 60 selected high-impact journal articles. The four themes are 1) examining the outcomes of corporate integrity and accountability practices; 2) evaluating the RNPOs’ internal control practices; 3) identifying financial reporting disclosures practices among RNPOs; and 4) exploring the influence of leadership skills on RNPOs’ accountability practices.
Planar vector fields with central symmetry: roughness and first degree of non-roughness
Authors: Ройтенберг Владимир Шлеймович 
Published: September 2021

Рассматривается пространство гладких векторных полей, заданных в замкнутой области D на плоскости, инвариантных относительно центральной симметрии и трансверсальных границе D. Описано множество векторных полей, грубых относительно этого пространства; показано, что оно открыто и всюду плотно. Во множестве всех негрубых векторных полей выделено открытое всюду плотное подмножество, состоящее из векторных полей первой степени негрубости.
We consider the space of smooth vector fields defined in a closed domain D on the plane, invariant under the central symmetry and transversal to the boundary D. The set of vector fields that are rough with respect to this space is described; it is shown that it is open and everywhere dense. In the set of all non-rough vector fields, an open everywhere dense subset consisting of vector fields of the first degree of non-roughness is distinguished.
Development of the malware detection model based on an analysis of API request sequences
Authors: Черкасов Александр Николаевич , Туркин Егор Алексеевич 
Published: September 2021

Анализ актуальности существующих работ по изучению нейросетевых алгоритмов обнаружения вредоносного программного обеспечения позволил определить оптимальный подход к решению задачи распознавания вирусов. Был сформирован набор данных, содержащий последовательности системных запросов для 2083 исполняемых файлов. Обучение модели рекуррентной нейронной сети на полученном наборе данных позволило получить классификатор с точностью распознавания вредоносных программ 97,6%. Ключевой аспект значимости работы заключается в практической ориентированности исследования - полученная модель будет применена в качестве компонента системы комплексного анализа вредоносного программного обеспечения.
An analysis of the relevance of existing works on the study of neural network algorithms for detecting malicious software made it possible to determine the optimal approach to solving the problem of virus recognition. A dataset has been generated containing sequences of system requests for 2083 executable files. Training the recurrent neural network model on the generated dataset made it possible to obtain a classifier with a malware recognition accuracy of 97.6%. The key aspect of the significance of the work lies in the practical orientation of the research - the resulting model will be applied as a component of a system for complex analysis of malicious software.
Chapter 9: Orogenic Gold Deposits of the Kibali District, Neoarchean Moto Belt, Northeastern Democratic Republic of Congo
Authors: Allibone Andrew , Vargas Carlos , Mwandale Etienne , Kwibisa Justus , Jongens Richard , Quick Sarah , Komarnisky Nathan , Fanning Mark , Bird Philip , MacKenzie Doug , Turnbull Rose , Holliday Joel 
Published: September 2021

Abstract
The Kibali district in the Democratic Republic of Congo hosts the large Karagba-Chaffeur-Durba (KCD) deposit and smaller satellite deposits that together contained 20 million ounces (Moz) of gold when mining recommenced in 2013. An additional 3 Moz of gold was probably mined from the district before 2013.
Gold deposits in the Kibali district are located along the KZ trend, a series of folds, contractional shear zones, and altered lithostratigraphic units that coincide with the margin of an earlier 2630 to 2625 Ma intraorogenic basin within the Neoarchean Moto belt. Fluids first responsible for barren carbonate-quartz-sericite alteration, and later for siderite and/or ankerite (±quartz, magnetite, pyrite, and/or chlorite) alteration with associated auriferous pyrite ± rare arsenopyrite veinlets, infiltrated and replaced the siliciclastic, banded iron formation (BIF), and chert host rocks via fold axes, shear zones, and reactive BIF horizons. The complex shape and gentle northeast plunge of the lodes across the Kibali district reflect the shape and plunge of coincident folds that formed during early barren alteration. Many other folded BIF horizons across the wider Moto belt remain barren or only weakly mineralized, suggesting deep extensional structures that may have developed in the vicinity of the KZ trend during basin opening and prior to gold mineralization, were important fluid pathways during later contractional deformation and mineralization.
Chapter 10: Olympiada Gold Deposit, Yenisei Ridge, Russia
Authors: Sazonov A. M. , Lobanov K. V. , Zvyagina E. A. , Leontiev S. I. , Silyanov S. A. , Nekrasova N. A. , Nekrasov A. Y. , Borodushkin A. B. , Poperekov V. A. , Zhuravlev V. V. , Ilyin S. S. , Kalinin Yu.A. , Savichev A. A. , Yakubchuk A. S. 
Published: September 2021

Abstract
The Olympiada deposit, containing &gt;1,560 metric tons (t; 50 Moz) of gold at an average grade of 4 to 4.6 g/t Au, occurs in central Siberia, Russia. Over 30 years, the deposit produced more than 580 t of gold, including 200 t from oxidized ore grading 11.1 g/t. The deposit forms a 2-km-long, steeply dipping system, which is traced downdip for 1.7 km. It occurs in the Neoproterozoic orogen of the Yenisei Ridge at the western margin of the Siberian craton. This and other gold deposits in the district are controlled by the large, long-lived Tatarka-Ishimbino tectonic zone, marking a suture between terranes chiefly consisting of deformed Meso- to Neoproterozoic carbonate-clastic sedimentary rocks. The combination of lithologic and structural factors was critical for localization of gold mineralization associated with calcic and siliceous alteration accompanied by early arsenic and late antimony sulfides. As a result, very fine (10 μm) and high fineness (910–997) gold associates with diverse sulfides, especially arsenopyrite, and commonly contains mercury, similar to some characteristics of Carlin-type deposits.
Geochronologic studies suggest that mineralization was formed during several stages between 817 and 660 Ma. The isotopic composition of Os and He, along with presence of anomalous Ni, Co, and Pt, points to a mantle mafic source, whereas isotopic composition of Pb and S suggest a contaminated crustal source, i.e., originating from a mix of mantle and crustal fluids.
Chapter 11: The Telfer Gold-Copper Deposit, Paterson Province, Western Australia
Authors: Wilson Alan J. , Lisowiec Nick , Switzer Cameron , Harris Anthony C. , Creaser Robert A. , Fanning C. Mark 
Published: September 2021

Abstract
The giant (&gt;20 Moz) Telfer Au-Cu deposit is located in the Paterson Province of Western Australia and is hosted by complexly deformed marine Neoproterozoic metasedimentary siltstones and quartz arenites. The Telfer district also contains magnetite- and ilmenite-series granitoids dated between ca. 645 and 600 Ma and a world-class W skarn deposit associated with the reduced, ~604 Ma O’Callaghans granite. Based on monazite and xenotime U-Pb geochronology, Telfer is estimated to be older than O’Callaghans, forming between 645 and 620 Ma.
Au-Cu mineralization at Telfer is hosted in multistage, bedding-parallel quartz-dolomite-pyrite-chalcopyrite reefs and related discordant veins and stockworks of similar composition that were emplaced into two NW-striking doubly plunging anticlines or domes. Mineralization is late orogenic in timing, with hot (≤460°C), saline (&lt;50 wt % NaCl equiv) ore fluids channeled into preexisting domes along a series of shallow, ENE-verging thrust faults and associated fault-propagated fold corridors. A combination of fault-propagated fold corridors acting as fluid conduits below the apex of the Telfer domes and the rheology and chemical contrast between interbedded siltstone and quartz arenite units within the dome are considered key parameters in the formation of the Telfer deposit.
Based on the presence of the reduced Au-Cu-W-Bi-Te-Sn-Co-As assemblage, saline and carbonic, high-temperature hydrothermal fluids in Telfer ore, and widespread ilmenite-series granites locally associated with W skarn mineralization, Telfer is considered to be a distal, intrusion-related gold deposit, the high copper content of which may be explained by the predominance of highly saline, magmatic fluids in gangue assemblages cogenetic with ore.
Chapter 14: The Brucejack Au-Ag Deposit, Northwest British Columbia, Canada: Multistage Porphyry to Epithermal Alteration, Mineralization, and Deposit Formation in an Island-Arc Setting
Authors: Board Warwick S. , McLeish Duncan F. , Greig Charles J. , Bath Octavia E. , Ashburner Joel E. , Murphy Travis , Friedman Richard M. 
Published: September 2021

Abstract
The Brucejack intermediate-sulfidation epithermal Au-Ag deposit, located 65 km north of Stewart, BC, forms part of a well-mineralized, structurally controlled, north-south gossanous trend associated with Early Jurassic intrusions straddling the Late Triassic-Early Jurassic Stuhini-Hazelton Group unconformity in the Sulphurets mineral district. Mining of the deposit commenced in mid-2017 after a long history of exploration dating back to the 1880s. Mineralization is hosted in deformed Lower Jurassic island-arc volcanic rocks of the Hazelton Group exposed on the eastern limb of the Cretaceous McTagg anticlinorium. High-grade Au-Ag mineralization was formed from ~184 to 183 Ma in association with a telescoped, multipulsed magmatic-hydrothermal system beneath an active local volcanic center. Precious metal mineralization occurs as coarse aggregates of electrum and silver sulfosalts in steeply dipping, E- to SE-trending quartz-carbonate vein stockwork zones cutting low-grade intrusion-related phyllic alteration. Epithermal vein development is interpreted to have occurred during the waning stages of Early Jurassic sinistral transpression in a compressive arc environment, followed by a limited Cretaceous deformation overprint.
Chapter 24: Muruntau, Uzbekistan: The World’s Largest Epigenetic Gold Deposit
Authors: Seltmann Reimar , Goldfarb Richard J. , Zu Bo , Creaser Robert A. , Dolgopolova Alla , Shatov Vitaly V. 
Published: September 2021

Abstract
Muruntau in the Central Kyzylkum desert of the South Tien Shan, western Uzbekistan, with past production of ~3,000 metric tons (t) Au since 1967, present annual production of ~60 t Au, and large remaining resources, is the world’s largest epigenetic Au deposit. The host rocks are the mainly Cambrian-Ordovician siliciclastic flysch of the Besapan sequence. The rocks were deformed into a broadly east-west fold-and-thrust belt prior to ca. 300 Ma during ocean closure along the South Tien Shan suture. A subsequent tectonic transition was characterized by left-lateral motion on regional splays from the suture and by a massive thermal event documented by widespread 300 to 275 Ma magmatism. The Besapan rocks were subjected to middle to upper greenschist-facies regional metamorphism, an overprinting more local thermal metamorphism to produce a large hornfels aureole, and then Au-related hydrothermal activity all during early parts of the thermal event. The giant Muruntau Au deposit formed in the low-strain hornfels rocks at ca. 288 Ma at the intersection of one of the east-west splays, the Sangruntau-Tamdytau shear zone, with a NE-trending regional fault zone, the Muruntau-Daugyztau fault, which likely formed as a cross fault during the onset of left-lateral translation on the regional splays. Interaction between the two faults opened a large dilational zone along a plunging anticlinorium fold nose that served as a major site for hydrothermal fluid focusing. The Au ores are dominantly present as a series of moderately to steeply dipping quartz ± K-feldspar stockwork systems surrounding uncommon central veins and with widespread lower Au-grade metasomatites (i.e., disseminated ores). Pervasive alteration is biotite-K-feldspar, although locally albitization is dominant. Sulfides are mainly arsenopyrite, pyrite, and lesser pyrrhotite, and scheelite may be present both in preore ductile veins and in the more brittle auriferous stockwork systems. The low-salinity, aqueous-carbonic ore-forming fluids probably deposited the bulk of the ore at 400° ± 50°C and 6-to 10-km paleodepth. The genesis of the deposit remains controversial with metamorphic, thermal aureole gold (TAG), and models related to mantle upwelling all having been suggested in recent years. More importantly, the question as to why there was such a focusing of so much Au and fluid into this one location, forming an ore system an order of magnitude larger than other giant Au deposits in metamorphic terranes, remains unresolved.
Chapter 25: The Sukhoi Log Gold Deposit, Russia
Authors: Vursiy G. L. , Zibrov I. A. , Lobov S. G. , Yakubchuk A. S. 
Published: September 2021

Abstract
Sukhoi Log, Russia’s largest gold deposit, containing 1,960 metric tons (t) of gold within the deformed Neoproterozoic sedimentary sequences of the Patom passive margin, can be classified as an orogenic gold system. This giant and nearby smaller deposits occur in black shale horizons at several stratigraphic levels.
The understanding of Sukhoi Log evolved from a small quartz vein occurrence to a large disseminated gold resource. The genesis of the deposit, originally considered to be related to a granitic intrusion, was later reinterpreted as metamorphogenic, with a significant contribution of synsedimentary gold in pyrite. Recent isotopic studies showed that there may have been more than one early Paleozoic synmetamorphic gold-mineralizing event, so the deposit most likely has a multistage origin.
Black shales might have acted either as a synsedimentary and/or synmetamorphic geochemical trap for auriferous fluids. Structurally, the mineralization is confined to the axial portion of the recumbent Sukhoi Log anticline, conjugate with the Kadali-Sukhoi Log shear zone. This imbricate thrust zone marks a major boundary between the Chuya-Nechera anticlinorium and Bodaibo synclinorium, two regional tectonic features in the Patom Highlands.
Chapter 28: Lihir Alkalic Epithermal Gold Deposit, Papua New Guinea
Authors: Cooke David R. , Sykora Stephanie , Lawlis Erin , Blackwell Jacqueline L. , Ageneau Mathieu , Jansen Nicholas H. , Harris Anthony C. , Selley David 
Published: September 2021

Abstract
The Lihir gold deposit, Papua New Guinea, is the world’s largest alkalic low-sulfidation epithermal gold deposit in terms of contained gold (50 Moz). The deposit formed over the past million years and records a progression from porphyry- to epithermal-style hydrothermal activity. The early porphyry stage was characterized by biotite-anhydrite-pyrite ± K-feldspar ± magnetite alteration and weak gold ± copper mineralization and produced abundant anhydrite ± carbonate veins and anhydrite ± biotite-cemented breccias. These features collectively characterize the deep-seated anhydrite zone at Lihir.
Several hundred thousand years ago, one or more catastrophic mass-wasting events unroofed the porphyry system after porphyry-stage hydrothermal activity ceased. Mass wasting may have been facilitated in part by dissolution of porphyry-stage anhydrite veins. Epithermal mineralization occurred after sector collapse, resulting in phreatic and hydraulic brecciation and veining, widespread adularia-pyrite ± carbonate alteration, and formation of mineralized zones at Lienetz, Minifie, Kapit, Kapit NE, Coastal, and Borefields. A NE- to ENE-striking fault array localized several of these orebodies. The pyrite-rich veins and pyrite-cemented breccias that formed during epithermal-stage hydrothermal activity define the sulfide zone at Lihir. This zone mostly contains refractory gold in pyrite, with minor free gold and precious metal tellurides hosted in late-stage quartz veins.
A period of diatreme volcanism disrupted the Luise amphitheater during the latter stages of epithermal mineralization. The diatreme breccia complex truncated several of the epithermal ore zones and was crosscut locally by late-stage epithermal veins. Recent geothermal activity produced a steam-heated clay alteration blanket that has overprinted the refractory sulfide-rich epithermal assemblage near the present-day land surface. Gold was remobilized downward from the steam-heated zone into the sulfide zone during argillic and advanced argillic alteration, producing thin gold-rich rims around pyrite grains. This process produced a high-grade tabular enrichment zone immediately beneath the base of the clay blanket.
Chapter 30: Geologic Evolution of Late Ordovician to Early Silurian Alkalic Porphyry Au-Cu Deposits at Cadia, New South Wales, Australia
Authors: Harris Anthony C. , Cooke David R. , Cuison Ana Liza Garcia , Groome Malissa , Wilson Alan J. , Fox Nathan , Holliday John , Tosdal Richard 
Published: September 2021

Abstract
The Cadia district of New South Wales contains four alkalic porphyry Au-Cu deposits (Cadia East, Ridgeway, Cadia Hill, and Cadia Quarry) and two Cu-Au-Fe skarn prospects (Big Cadia and Little Cadia), with a total of ~50 Moz Au and ~9.5 Mt Cu (reserves, resources, and past production). The ore deposits are hosted by volcaniclastic rocks of the Weemalla Formation and Forest Reefs Volcanics, which were deposited in a submarine basin on the flanks of the Macquarie Arc during the Middle to Late Ordovician. Alkalic magmatism occurred during the Benambran orogeny in the Late Ordovician to early Silurian, resulting in the emplacement of monzonite intrusive complexes and the formation of porphyry Au-Cu mineralization. Ridgeway formed synchronous with the first compressive peak of deformation and is characterized by an intrusion-centered quartz-magnetite-bornite-chalcopyrite-Au vein stockwork associated with calc-potassic alteration localized around the apex of the pencil-like Ridgeway intrusive complex. The volcanic-hosted giant Cadia East deposit and the intrusion-hosted Cadia Hill and Cadia Quarry deposits formed during a period of relaxation after the first compressive peak of the Benambran orogeny and are characterized by sheeted quartz-sulfide-carbonate vein arrays associated with subtle potassic, calc-potassic, and propylitic alteration halos.
Pengaruh Metode Cirkuit Training Terhadap Kecepatan Pemanjatan Wallclimbing Atlet Federasi Panjat Tebing Indonesia (FPTI) Dalam Jalur Speed Word Record
Authors: Saputra Arry , Henjilito Raffly 
Published: September 2021

Kurang teroganisasinya latihan pada altet Federasi Panjat Tebing Indonesia (FPTI) kota Pekanbaru saat latihan yang hanya berlatih secara individual tanpa program latihan yang jelas sehingga hasil yang diinginkan kurang tercapai secara maksimal
Berdasarkan uraian di atas penulis tertarik untuk melakukan penelitian dengan judul ’’ Pengaruh Metode Cirkuit Training Terhadap Kecepatan Pemanjatan Wallclimbing Atlet Federasi Panjat Tebing Indonesia (FPTI) Dalam Jalur Speed Word Record Kota Pekanbaru’’.