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

Поиск по книгам
Автор(ы):Sinclair W.D.
Издание:2007 г., 21 стр.
Язык(и)Английский
Porphyry deposits / Порфировые месторождения

Porphyry deposits are the world's most important source of Cu and Mo, and are major sources of Au, Ag, and Sn; significant byproduct metals include Re, W, In, Pt, Pd, and Se. They account for about 50 to 60% of world Cu production and more than 95% of world Mo production. In Canada, they account for more than 40% of Cu production, virtually all Mo production, and about 10% of Au production. Porphyry deposits are large, low- to medium-grade deposits in which primary (hypogene) ore minerals are dominantly structurally controlled and which are spatially and genetically related to felsic to intermediate porphyritic intrusions.

Издание:PGS Publishing, Linden Park, 2005 г., 10 стр.
Язык(и)Английский
Porphyry-style mineralisation in the Ertsberg diorite, Gunung Bijih (Ertsberg/Grasberg) district, West Papua, Indonesia

Newly-recognised porphyry-style mineralisation within the Ertsberg intrusion displays significant differences from porphyry mineralisation at the Grasberg porphyry Cu-Au deposit. Stockwork mineralisation in the Ertsberg occurs near the giant East Ertsberg Skarn System, close to the northern margin of the intrusion. Stockwork mineralisation in the diorite is spatially associated with 5-15 m wide, E-striking, dykes of porphyritic hornblende monzonite that cut equigranular Ertsberg diorite. The porphyry dykes strike parallel to major district structures and occur where those structures project into the Ertsberg intrusion. Hornblende abundance greater than biotite, the much greater content of sphene, a paucity of broken phenocrysts, and the aplitic groundmass distinguish the porphyry dykes in the Ertsberg Stockwork Zone from the finer-grained groundmass Kali dykes of the Grasberg deposit.

Автор(ы):Talusani R.V.R.
Издание:Journal Ore geology reviews, 2001 г., 7 стр.
Язык(и)Английский
Possible Carlin-type disseminated gold mineralization in the Mahakoshal fold belt, central India

The paper records the first occurrence of dolomite-hosted, disseminated gold mineralization at Barhi and Jhal, in a Late Archean-Early Proterozoic metavolcano-sedimentary belt ŽMahakoshal fold belt. in central India. Gold mineralization is hosted by dolomite that occurs as discontinuous bands interbedded with phyllite. Hydrothermal alteration styles of the host rock include decalcification, silicification, and argillization. Pyrite is the most common sulfide, whereas stibnite and realgar are rare. Mineralization is characterized by persistent gold from 0.20 to 0.62 ppm and a consistent association of anomalous arsenic, antimony, and mercury with gold.

Автор(ы):Kummel B.
Издание:Bulletin of the museum of Comparative zoology, Cambridge, 1956 г., 233 стр.
Язык(и)Английский
Post-triassic nautiloid genera

Studies on tetrabranchiate cephalopods have added much data to our understanding of the patterns and modes of evolution as displayed by fossil animals. Few invertebrate phyla show such marked periods of expansion in evolutionary intensity contrasted with periods of extreme contraction to the point of near extinction. The generalized evolutionary history of the ammonoids with periods of near extinction at the end of the Paleozoic and again at the end of the Triassic, and their final extinction at the end of the Cretaceous is well known. Among the nautiloid cephalopods a similar evolutionary history exists but with some important differences <...>

Автор(ы):Roy K.K.
Издание:Springer, 2008 г., 670 стр., ISBN: 978-3-540-721089-8
Язык(и)Английский
Potential Theory in Applied Geophysics / Теория потенциалов в прикладной геофизике

Since foundation of potential theory in geophysics is based on scalar and vector potentials, a brief introductory note on vector analysis is given. Besides preliminaries of vector algebra, gradient divergence and curl are defined. Gauss’s divergence theorem to convert a volume integral to a surface integral and Stoke’s theorem to convert a surface integral to a line integral are given. A few well known relations in vector analysis are given as ready references.

Автор(ы):Hencher S.
Издание:Spon Press, 2012 г., 465 стр., ISBN: 978-0-415-46908-1
Язык(и)Английский
Practical engineering geology / Практическая инженерная геология

Geology can be defined as the scientific study of the Earth and especially the rocks and soils that make up the Earth: their origins, nature and distribution, and the processes involved in their formation. Engineering geology then may be defined as the scientific study of geology as it relates to civil engineering projects such as the design of a bridge, construction of a dam or preventing a landslide. Engineering geologists need to identify the local rock and soil conditions at a site and anticipate natural hazards such as earthquakes so that structures can be designed, constructed and operated safely and economically. He (or she, throughout) needs to work with civil engineers and understand what they are trying to do and the constraints under which they work. His remit and responsibilities can be extensive, covering all of the Earth Sciences, including geophysics, geochemistry and geomorphology. <...>

Издание 2
Автор(ы):Hencher S.
Издание:CRC Press, 566 стр., ISBN: 978-1-032-39225-7
Язык(и)Английский
Practical engineering geology / Практическая инженерная геология

The engineering geologist should be able to identify soil and rocks by visual examination and to interpret the geological history and structure of a site as set out in Chapter 4. He needs to be able to describe these rocks and soils both geologically and, in an unambiguous way, in terms of their relative strengths. He also must have knowledge of geomorphological processes, be able to interpret terrain features and hydrogeological conditions. Principles of hydrogeology are dealt with in Chapter 5.

Автор(ы):Clark I.
Издание:2001 г., 119 стр.
Язык(и)Английский
Practical geostatistics / Практическая геостатистика

This book is aimed at postgraduates, undergraduates and workers in industry who require an introduction to geostatistics. It is based on seven years of courses to undergraduates, M.Sc. students and short courses to industry, and reflects the problems which have been encountered in presenting this material to mining engineers and geologists over a wide age range, and with an equally wide range of numerical ability. The book would provide the foundation of a course of about 20 to 30 hours, or of a five-day short course.

Автор(ы):Clark I.
Издание:Elsevier, 1987 г., 129 стр., ISBN: 0-85334-843-X
Язык(и)Английский
Practical geostatistics / Практическая геостатистика
1652.86