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Издание 3
Автор(ы):Bradley R.S.
Издание:Elsevier, 2015 г., 676 стр., ISBN: 978-0-12-386913-5
Язык(и)Английский
Paleoclimatology. Reconstructing climates of the quaternary / Палеоклиматология. Реконструкция климатов четвертичного периода

Earth is a constantly changing dynamic entity, composed of multiple complex physical, chemical, and biological systems that interact on a spectrum of time and spatial scales. To comprehend the Earth System as a whole, we must understand the nature of these complex subsystems, both now and in the past, and identify the important linkages among them. Earth is now experiencing many changes, some large and more rapid than others.

Автор(ы):Tauxe L.
Издание:Kluwer Academic Publishers, 2003 г., 300 стр., ISBN: 0-306-48128-6
Язык(и)Английский
Paleomagnetic principles and practice / Принципы и практица палеомагнтиных исследований

Paleomagnetic data are useful in many applications in Earth Science from determining paleocurrent directions to analyzing the long-term behavior of the geomagnetic field. Despite the diversity of applications, the techniques required to obtain and analyze the data are similar. This book attempts to draw together the various principles and practices within paleomagnetism in a consistent and up-to-date manner. It was written for several categories of readers:
1)    for Earth Scientists who use paleomagnetic data in their' research,
2)    for students taking a class with paleomagnetic content, and
3)    for other professionals with an interest in paleomagnetic data. <...>

Автор(ы):McElhinny M.W., McFadden P.L.
Издание:Academic Press, 2000 г., 406 стр., ISBN: 0-12-483355-1
Язык(и)Английский
Paleomagnetism. Continental and oceans / Палеомагнетизм. Континенты и океаны

This book is the sequel to Palaeomagnetism and Plate Tectonics written by Michael W. McElhinny, first published in 1973. The aim of that book was to explain the intricacies of paleomagnetism and of plate tectonics and then to demonstrate that paleomagnetism confirmed the validity of the new paradigm. Today it is no longer necessary to explain plate tectonics, but paleomagnetism has progressed rapidly over the past 25 years. Furthermore, magnetic anomaly data over most of the oceans have been analyzed in the context of sea-floor spreading and reversals of the Earth's magnetic field. Oceanic data can also be used to determine paleomagnetic poles by combining disparate types of data, from deep-sea cores, seamounts, and magnetic anomalies. Our aim here is to explain paleomagnetism and its contribution in both the continental and the oceanic environment, following the general outline of the initial book. We demonstrate the use of paleomagnetism in determining the evolution of the Earth's crust. <...>

Редактор(ы):Carvalho I. de S.
Издание:2010 г., 735 стр., ISBN: 978-85-7193-224-1
Язык(и)Английский
Paleontologia. Conceitos e Metodos / Палеонтология. Понятия и методы
Автор(ы):Weaver C.E.
Издание:University of Washington press, Washington, 1931 г., 598 стр.
Язык(и)Английский
Paleontology of the jurassic and cretaceous of west central Argentina / Палеонтология юрского и мелового периодов западно-центральной Аргентины

Early in the Mesozoic the western portion of the South American continent was subjected to differential but gentle crustal deformation which resulted in a series of crustal downwarps situated at intervals from Colombia on the north to Southern Patagonia on the south. These downwarps were in the nature of small geosynclinal troughs separated one from the other by peninsula-like land areas of probable low topographic relief.

Автор(ы):Bainbridge D.
Издание:Quarto Publishing plc, 2022 г., 256 стр., ISBN: 978-0-691-22092-5
Язык(и)Английский
Paleontology. An illustrated history / Палеонтология. Иллюстрированная история

Writing this history of paleontology has revived vivid fossil-related memories from my past. Ever since childhood I have been fascinated and inspired by the fragmentary vestiges of ancient creatures, the rubble of once great nations of animals.
Every birthday I would plead with my parents to be taken to the Natural History Museum in London, in a more naive era when a small boy could be set free to explore the terracotta halls of this Romanesque “cathedral of life.” I loved the grand dinosaur skeletons, of course, although I was already aware that some of them were made of plaster, but it was the unfrequented gallery of ancient fish that I remember most. Even more than their spectacular land-living descendants, this gallery’s inhabitants looked intriguingly, overwhelmingly old—crushed and mangled messengers from an alien era before feet trod the Earth. Many appeared timid and harmless, yet some were heavily armored, hinting that some awful threat was abroad in those days. <...>

Автор(ы):Uffmann A.K.
Издание:2013 г., 173 стр.
Язык(и)Английский
Paleozoic petroleum systems of northern Germany and adjacent  areas: A 3D modeling study / Палеозойские нефтяные системы севера Германии и прилегающих территорий: исследования 3D моделированием

First of all I would like to express my deep gratitude towards Prof. Dr. rer. nat. Ralf Littke for giving me the opportunity to carry out my PhD studies at the Institute of Geology and Geochemistry of Petroleum and Coal and for his constant support throughout my studies and personal development.

Том 19, Выпуск 3/4
Издание:Pergamon, 1995 г., 22 стр.
Язык(и)Английский
Paleozoic transcurrent conjugate shear zone in the central Appalachian Piedmont of Southeastern Pennsylvania

Well-documented tectonic events in the central Appalachians of Pennsylvania are: (1) the early Paleozoic Taconian orogeny that occurred during convergence of Laurentian and the Chopawamsic-Wilmington complex magmatic arc over an east-dipping subduction zone, and resulted in intense metamorphism and deformation in the Piedmont, and (2) the late Paleozoic Alleghanian orogeny that resulted in the thrust and fold belt in the Valley and Ridge province and dextral shear zones in the Piedmont. Unlike the Paleozoic tectonic history for the northern and southern Appalachians, the north-central part of the orogen in Pennsylvania lacks evidence for Acadian deformation and metamorphism. The relative chronological order of deformation and metamorphic events in the eastern Piedmont of Pennsylvania, combined with published geochro-nology suggests the previously undocumented Acadian deformation possibly exists as a transcurrent conjugate shear zone pair.

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