Добрый день, Коллеги. Важное сообщение, просьба принять участие. Музей Ферсмана ищет помощь для реставрационных работ в помещении. Подробности по ссылке
Рассматриваются общие и региональные вопросы стратиграфии, палеонтологии, литологии, палеогеографии докембрия и фанерозоя различных областей Восточно-Европейской и Сибирской древних платформ, Урало-Монгольского, Тихоокеанского и Средиземноморского геосинклинальноскладчатых поясов.
Розен О. М., Невский Л. К., Журавлев Д. 3., Ротман А. Я., Специус3. В., Макеев А. Ф., Зинчук Н. Н., Манаков А. В., Серенко Б. Я. Палеопротерозойская аккреция на северо-востоке Сибирского кратона: изотопное датирование Анабарской коллизионной системы Кузнецов А. Б., Семихатов М. А., Маслов А. В., Горохов И. М., Прасолов Э. М., Крупенин М. Г., Кислова И. В. Sr- и С -изотопная хемостратиграфия типового разреза верхнего рифея (Южный Урал): новые данные Шевырев А. А. Биохронология триаса: современное состояние и основные проблемы Лобачева С. В., Смирнова Т. Н. Комплексы брахиопод берриаса Крыма Вангенгейм Э. А., Лунгу А. Н., Тесаков А. С. Возраст нижней границы валлезия (континентальный миоцен Европы) Запорожец Н. И., Синельникова В. Н., Ахметъев М. А. Органикостенный фитопланктон палеогена разрезов Западной Камчатки Шлезингер А. Е., Гладенков Ю. Б., Захаров В. А. К оценке новых методических приемов секвенс-стратиграфического анализа Негруца В. 3. Стратиграфия архея на I Российской конференции по проблемам геологии и геодинамики докембрия Памяти Артура Хасенбековича Кагарманова (1934-2005)
This book has been written to bring up to date The Interior of the Earth, published in 1971 following the plate tectonic revolution. Plate tectonic theory has now been widely accepted as a unifying theory for the origin ofthe Earth’s major surface features, and the broad viewpoint taken in 1971 has been vindicated. The last ten years, however, has been a period of continuing rapid advance in earth sciences. The structure of the Earth’s interior has become much better defined. A new understanding ofthe physical processes within the Earth which permit the escape of heat from the deep interior, drive the geomagnetic dynamo and cause the plate motions, is emerging. Consequently, much of the original text has had to be re-written to produce this new book.
This is the first book to deal comprehensively with Spain's tectonic and sedimentary history over the past sixty or so million years. During these Tertiary times, Spain has suffered compressional collision between France and Africa, and its Atlantic and Mediterranean coasts have been further modified by extensional rifting. This study will therefore be of interest to earth scientists generally because of the insights it provides into continental crustal deformation. Spain contains some of the best exposed outcrop geology in Europe.
Scientists, in general, tend to be reticent in calling attention to their contributions to science. Satisfaction comes from the solution of a problem rather than from any public acclaim they may receive. Once a paper is presented, there is generally reluctance to present it again. The true scientist is never satisfied with past results, and is constantly attacking new problems. He is an entrepreneur in the finest sense of the word, and at the same time a religious zealot in his dedication to his work, and a visionary in his concentration on the unknown. It is, therefore, not surprising that scientists and churchmen have many characteristics in common; that churchmen through the ages have made significant contributions to the advance of science; and that scientists and churchmen, individually, are 'warm' human beings more concerned with their work and others than with themselves.
The initiative for this Memoir arose from a series of field-based geological studies in Sumatra by the Institute of Geological Sciences (later the British Geological Survey) and the University of London Group for Geological Research in Southeast Asia in collaboration with the Indonesian Ministry of Mines, through the Geological Research and Development Centre and the Directorate of Mineral Resources in Bandung, and the Research and Development Centre for Oil and Gas Technology (LEMIGAS) in Jakarta between 1975 and 1995. The Indonesian side selected Sumatra as a suitable area for this programme of scientific and technical assistance in geological, geochemical and geophysical surveys, inventories of mineral potential and the training of geoscientists in pursuance of successive five-year development plans (Pelita). The work culminated in the publication by the Geological Research and Development Centre of a series of 42 1:250 000 Geological Map Sheets with Explanatory Notes covering the whole of Sumatra. In compiling these geological maps the work of the Dutch geologists of the Netherlands Indies Geological Survey, who commenced a systematic programme of mapping in Sumatra before the Second World War, and the work of geologists working for oil companies with concessions in Sumatra, supported by the Indonesian National Oil Company (Pertamina), and published since 1971 in the Proceedings of the Indonesian Petroleum Association, were also incorporated.
The study of seismic wave propagation, especially of the P (longitudinal) waves, has enabled us to distinguish two components in the shallower part of the earth:
- The crust (thickness varying from 10 to 70 km, average 30 Ian);
- The underlying mantle, separated from the crust by a surface of discontinuity at which the seismic-wave velocities change suddenly (the Mohorovicic discontinuity, generally shortened to Moho).
Данные методические указания предназначены для студентов 3 курса для дневного отделения факультета природных ресурсов ГОУ ОГУ. В них, в соответствии с программой курса «Региональная геология» и учебным планом факультета, изложено содержание лабораторных занятий по следующему разделу: Геологическое строение территории России и стран ближнего зарубежья.
