B.A. Roberts; J. Proctor The Ecology of Areas with Serpentinized Rocks 9789401056540

Варианты приобретения

Цена: 16979.00р.
Кол-во:
Наличие: Поставка под заказ. Есть в наличии на складе поставщика.
Склад Америка: Есть
При оформлении заказа до: 2025-09-15
Ориентировочная дата поставки: Октябрь
При условии наличия книги у поставщика.

Добавить в корзину

в Мои желания

Автор: B.A. Roberts; J. Proctor
Название: The Ecology of Areas with Serpentinized Rocks
ISBN: 9789401056540
Издательство: Springer
Классификация:

Ботаника и науки о растениях

Экология растений

Геология и литосфера

Почвоведение, седиментология

ISBN-10: 9401056544
Обложка/Формат: Soft cover
Страницы: 429
Вес: 1.09 кг.
Дата издания: 22.11.2012
Серия: Geobotany
Язык: English
Издание: Softcover reprint of
Иллюстрации: Colour illustrations, bibliography
Размер: 279 x 210 x 23
Читательская аудитория: Professional & vocational
Основная тема: Plant Sciences
Подзаголовок: A World View
Ссылка на Издательство: Link
Рейтинг:
Поставляется из: Германии
Описание: B. A. ROBERTS&J. PROCTOR The term serpentine referring to rocks and min- of each of the polymorphs. These conditions in- erals, can be traced back to the ancient Roman clude temperatures of generally less than 530C, era of Dioscorides (A. D. 50) (Faust & Fahey and fluid pHs in excess of 10 with low pC02- Serpentine protoliths are essentially ultramafic 1962) and they suggest that the speckled colour of serpents and the fact that Dioscorides recom- rocks which fall into a number of categories: (a) mended it for the prevention of snakebite as two stratiform complexes, (b) concentrically zoned complexes, (c) ophiolite complexes and, (d) high- of many origins of the name. It is well known that the use of serpentinized rocks by sculptors temperature peridotite complexes. The most and carvers since ancient times is a tradition that commonly recognized are generally assigned to the ophiolite suite (Malpas, Ch. 2, this is still carried on today (Fig. 1). The differences in chemical composition of serpentinized rocks volume) and occur in most fold-mountain belts are many and specimens come in a wide range of of the world. Serpentinized ultramafic rocks attractive solid and mixed colours, e. g., red, H4(MgFe hSi20 9, approximate composition) green, blue and black.

The Ecology of Areas with Serpentinized Rocks, B.A. Roberts; J. Proctor