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Редактор(ы):Bai M., Shen X., Standifird W.
Издание:CRC Press, 2011 г., 239 стр., ISBN: 978-1-4398-7055-6
Язык(и)Английский
Drilling and completion in petroleum engineering. Theory and numerical applications / Бурение и заканчивание в нефтяных скважин. Теория и численные приложения

Numerical modeling is the process of obtaining approximate solutions to problems of scientific and/or engineering interest. The book series addresses novel mathematical and numerical techniques with an interdisciplinary emphasis that cuts across all fields of science, engineering and technology. It focuses on breakthrough research in a richly varied range of applications in physical, chemical, biological, geoscientific, medical and other fields in response to the explosively growing interest in numerical modeling in general and its expansion to ever more sophisticated physics. The goal of this series is to bridge the knowledge gap among engineers, scientists, and software developers trained in a variety of disciplines and to improve knowledge transfer among these groups involved in research, development and/or education. <...>

Автор(ы):Prassl W.F.
Издание:Curtin University of Technology, 281 стр.
Язык(и)Английский
Drilling Engineering / Технология бурения

This text aims to give students an introduction to the principles and some recommended procedures practiced in drilling engineering. All chapters contain a theoretical introduction, as well as examples and exercises. References for further readings are given at the end of this text. Necessary equations and procedures to solve the exercises are presented through out the text <...>

ТематикаБурение
МеткиБурение (645)
Автор(ы):Adams N.J.
Издание:Pennwell Books, 1985 г., 848 стр., ISBN: 0-87814-265-7
Язык(и)Английский
Drilling engineering. A complete well planning approach / Проектирование бурения. Комплексный подход к планированию скважины

Many people and companies must be acknowledged for their assistance in the preparation of this book. Undoubtably, I will fail to mention all of them. To them 1 sincerely apologize for the oversight.

Издание:McGraw-Hill Book Company, 2022 г., 963 стр., ISBN: 978-1-259-64374-3
Язык(и)Английский
Drilling mechanics. Advanced applications and technology / Механика бурения. Передовые методы применения и технологии

The history of well drilling goes back for millennia. Oilwell drilling has, even to this day, been more a craft rather than an engineering science. An engineering approach to oilwell drilling first began to take hold at the end of World War II. Perhaps one indication was seven papers related to drilling and completion topics in the 1953 Transactions of the AIME, Petroleum  Development and Technology.

Автор(ы):Riquelme A.I.
Издание:2024 г., 35 стр.
Язык(и)Английский
Dual random fields and their application to mineral potential mapping / Двойные случайные поля и их применение для картирования потенциала полезных ископаемых

In various geosciences branches, including mineral exploration, geometallurgical characterization on established mining operations, and remote sensing, the regionalized input variables are spatially well-sampled across the domain of interest, limiting the scope of spatial uncertainty quantification procedures. In turn, response outcomes such as the mineral potential in a given region, mining throughput, metallurgical recovery, or in-situ estimations from remote satellite imagery, are usually modeled from a much-restricted subset of testing samples, collected at certain locations due to accessibility restrictions and the high acquisition costs.

Редактор(ы):Mukherjee S., Mulchrone K.F.
Издание:Wiley Blackwell, 2016 г., 625 стр., ISBN: 978-1-118-84496-0
Язык(и)Английский
Ductile shear zones. From mcro- to macro-scales / Зоны пластичного сдвига. От микро- к макромасштабам

Heterogeneous ductile shear zones are very common in the Earth’s lithosphere and are particularly well exposed in mountain belts (e.g. Iannace and Vitale 2004; Yonkee 2005; Vitale et al. 2007a,b; Okudaira and Beppu 2008; Alsleben et al. 2008; Sarkarinejad et al. 2010; Kuiper et al. 2011; Dasgupta et al. 2012; Zhang et al. 2013; Samani 2013; Mukherjee 2013, 2014; also see Chapter 9), where they provide useful tools for a better understanding of the processes and parameters controlling strain localization, type of deformation, and rock rheology. The occurrence of strain markers such as fossils, ooids and ellipsoidal clasts in sedimentary rocks, or equant minerals, deflected veins and dykes in igneous rocks, allows one to quantify the finite strain by means of various methods (e.g. Dunnet 1969; Fry 1979; Lisle 1985; Erslev 1988; Vitale and Mazzoli 2005, 2010). <...>

Издание:Springer, 2019 г., 500 стр., ISBN: 978-981-13-1665-4
Язык(и)Английский
Dyke Swarms of the World: A Modern Perspective / Рои даек в мире: современные перспективы

Detailed multidisciplinary studies on mafic dyke swarms play a crucial role in solving geodynamic problems of Earth’s history. Professor Henry C. Halls recognized the importance of dyke swarms long ago and organized the first International Dyke Conference focusing on geological, geochemical, and geophysical aspects of dykes and related units in Toronto, Canada, in 1985. Given the new insights arising during that conference, it was decided that International Dyke Conferences (IDCs) should be held every 5 years. Consequently, IDC-2 was held in Australia in 1990, IDC-3 in Israel in 1995, IDC-4 in South Africa in 2001, IDC-5 in Finland in 2005, and IDC-6 in India in 2010. Each IDC also produced a proceedings volume (apart from IDC-4 whose contributions were published as part of the IDC-5 volume) (Halls and Fahrig 1987; Parker et al. 1990; Baer and Heimann 1995; Hanski et al. 2006; Srivastava 2011).<...>

Редактор(ы):Hanski E., Mertanen S., Ramo T., Vuollo J.
Издание:Taylor & Francis Group, 2006 г., 533 стр., ISBN: 978-0-415-39899-2
Язык(и)Английский
Dyke swarms – time markers of crustal evolution / Рои даек – временные маркеры эволюции земной коры

Short-lived mantle generated magmatic events and their dyke swarms: The key unlocking Earth’s palaeogeographic record back to 2.6 Ga 

W. Bleeker & R. Ernst

Giant dyke swarms and the reconstruction of the Canadian Arctic islands, Greenland, Svalbard and Franz Josef Land 

K.L. Buchan & R. Ernst

AMS criteria for determining the azimuth and dip of a subduction zone from a mafic dyke swarm 

J.-P. Lefort, T. Aпfa & F. Hervй

Palaeo- and Mesoproterozoic dyke swarms in the Lake Ladoga area, NW Russia – palaeomagnetic studies 

S. Mertanen, O. Eklund, A. Shebanov, D. Frank-Kamenetsky & T. Vasilieva

Автор(ы):Davies G.F.
Издание:Cambridge University Press, 1999 г., 469 стр., ISBN: 0-521-59067-1
Язык(и)Английский
Dynamic Earth. Plates, plumes and mantle convection / Динамичная Земля. Плиты, плюмы и мантийная конвекция

Dynamic Earth presents the principles of convection in the earth's mantle in an accessible style. Mantle convection is the process underlying plate tectonics, volcanic hotspots and, hence, most geological processes. This book is one of the first to synthesise the exciting insights into the earth's basic internal mechanisms that have flowed from the plate tectonics revolution of the 1960s.

Редактор(ы):Vetere F.
Издание:Wiley, 2021 г., 210 стр., ISBN: 978-111-952-1136
Язык(и)Английский
Dynamic Magma Evolution / Динамическая эволюция магмы

The rates and timescales of crustal magma transfer, storage, emplacement, and eruption are a key to understanding subvolcanic processes, characterizing volcanic hazards, and developing mitigation strategies. In this chapter, we review the most pertinent open questions in this field, as well as the many geochemical and geophysical methods that are available to address these questions. Results point to long storage timescales, of up to ~106 years, in deep (i.e., ~20–30 km), crustal hot zones. Estimated ascent velocities from deep reservoirs to shallower systems span a vast range of ~10 orders of magnitude, and are a function of the thermophysical parameters of the ascending magma (e.g., density, viscosity, and overpressures in the reservoirs) and the host rocks. At mid‐ to upper crustal levels (i.e., < 15–20 km), we elucidate the cold storage of magma mushes for long periods, which can be unlocked during short‐term events to form ephemeral magma chambers. Unlocking timescale estimates range from minutes to thousands of years, indicating a variability of about ~8 to ~10 orders of magnitude.

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