Добрый день, Коллеги. Важное сообщение, просьба принять участие. Музей Ферсмана ищет помощь для реставрационных работ в помещении. Подробности по ссылке

Поиск по книгам
Издание:Deswik, 2010 г., 85 стр.
Язык(и)Английский
Deswik.IS for open pits introductory training manual / Deswik.IS для открытых горных работ. Вводный курс

The following process flow illustrates the steps required to complete an open pit design by either slicing the pit into Bench’s by Elevations, or doing more detailed design and breaking it out into blast polygons <...>

Издание:2022 г., 97 стр.
Язык(и)Английский
Deswik.IS. Dependencies for underground metals / Зависимости при подземной отработке полезных ископаемых

Azimuth and gradient search parameters allow the user to define the search direction of the spatial link. Azimuth search parameters can be used to link from undercut rings to first task in drawpoint drive using defined azimuth search direction, this will drive the direction of the SLC front. Gradient search parameters are similar, an example being stope linking in narrow vein steeply dipping stopes. <...>

Автор(ы):Peck W.
Издание:2000 г., 4 стр.
Язык(и)Английский
Determining the stress reduction factor in highly stressed jointed rock / Определение коэффициента снижения напряжений в высоконапряженных трещиноватых породах

A number of Australian underground mines are using empirical rating systems to characterize the ground conditions in developmental headings for geotechnical design. The two best-known rating systems are Barton’s Rock Tunnelling Quality Index (Q-System, also known as the NGI System) and Bieniawski’s Rock Mass Rating (RMR, also known as the Geomechanics Classification). As the RMR makes no allowance for high ground stresses at depth, Barton’s Q-System is more likely to be used in deep Australian underground mines. The Q-value is determined from equation 1 using the six parameters listed in table 1. The numerical value of Q ranges from 0.001 (exceptionally poor) to 1000 (exceptionally good) quality rock. <...>

Редактор(ы):Bernet M., Spiegel C.
Издание:Geology Society of America, 2004 г., 131 стр., ISBN: 0-8137-2378-7
Язык(и)Английский
Detrital thermochronology—Provenance analysis, exhumation, and landscape evolution of mountain belts / Детритовая термохронология - анализ происхождения, эксгумация, и ландшафтная эволюция горных поясов

In recent years, an increasing number of studies have used single-grain age dating of detrital sediments to obtain information on sediment provenance, the thermal history and exhumation of sediment source areas, and landscape evolution. In order to highlight the value of this current development in geological research, we based this volume on papers presented in a session on detrital thermochonology at the 2002 Geological Society of America Annual Meeting held in Denver, Colorado. This Special Paper provides a short overview of the different, nowadays commonly used, dating techniques in detrital thermochronology, followed by discussion of some of the methodological aspects of detrital thermochronology (in the first two manuscripts) and of a variety of applications of detrital thermochronology, demonstrated in several regional case studies. <...>

Редактор(ы):Morton-Thompson D., Woods A.M.
Издание:American Association of Petroleum Geologists, 1992 г., 549 стр., ISBN: 0-89181-660-7
Язык(и)Английский
Development geology reference manual / Справочное руководство по промысловой геологии

The United States and the individual states have followed a legal system based on Roman law, which allows private ownership of oil and gas interests. Nevertheless, the federal and state governments control the leasing of about one-third of the oil and gas interests underlying the onshore landmass of the United States (estimated at 2.2 billion acres). They also control 100% (97% federal and 3% state) of the offshore areas of the United States (estimated at 885.6 million acres). In additional, 54 million acres of Indian lands are subject to U.S. government leasing control, and leasing rights to 44 million acres in Alaska are controlled by Alaskan natives (Mineral Management Service, 1989; Petroleum Independent, 1991). <...>

Издание:Bochum, 2005 г., 93 стр.
Язык(и)Английский
Development of pull-apart basins and associated structures by the riedel shear mechanism: insigth from scaled clay analogue models / Разработка бассейнов пул-апарт и связанных с ними структур с помощью механизма сдвига Риделя: выводы из моделирования

The physical and mechanical properties of clay materials required to scale the tectonic analogue experiments are analysed based on the modern soil mechanics concepts. A practical procedure for the determination of these properties is presented. Scaled clay experiments under Riedel shear mechanism produced a series of typical pull-apart structures. At the initial stages of the development of the deformation zone within the clay slab, the synthetic shear fractures (Riedel shears) display dilatational behaviour.

Редактор(ы):Bliss J.D.
Издание:2004 г., 26 стр.
Язык(и)Английский
Developments in mineral deposit modeling / Развитие моделирования месторождений полезных ископаемых

Activities in mineral deposit modeling have continued to develop on several fronts since the publication of “Mineral Deposit Models,” edited by Cox and Singer (1986). That bulletin is a collection of 87 descriptive deposit models and 60 grade and tonnage models prepared by many authors both from within and outside of the U.S. Geological Survey. The present bulletin continues that effort with the addition of new or revised models. Before these models are introduced, a review of modeling as used here is provided as well as an overview of mineral deposit modeling since the publication of Cox and Singer (1986).

Автор(ы):Pollard L.D., Weaver C.
Издание:Elsevier, 1973 г., 221 стр., ISBN: 0-444-41043-0
Язык(и)Английский
Developments in sedimentology. Volume 15. The chemistry of clay minerals / Исследования в седиментологии. Том 15. Химия глинистых минералов

Clay minerals occur in all types of sediments and sedimentary rocks and are a common constituent of hydrothermal deposits. They are the most abundant minerals in sedimentary rocks perhaps comprising as much as 40% of the minerals in these rocks. Half or more of the clay minerals in the earth's crust are illites, followed, in order of relative abundance, by montmorillonite and mixed-layer illite-montmorillonite, chlorite and mixed-layer chlorite-montmorillonite, kaolinite and septachlorite, attapulgite and sepiolite. The clay minerals are fine-grained. They are built up of tetrahedrally (Si, A l , Fe3+) and octahedrally (Al, Fe3+, Fez+, Mg) coordinated cations organized to form either sheets or chains. All are hydrous. <...>

2019.82