Minerals are intrinsically resistant to the processes that homogenize silicate liquids—their compositions thus yield an archive of volcanic and magmatic processes that are invisible at the whole rock scale. Minerals and their inclusions record diverse magma compositions, the depths and temperatures of magma storage, the nature of open system processes, and the rates at which magmas ascend.

The Middle Miocene Orduzu volcanic suite, which is a part of the widespread Neogene Yamadag˘ volcanism of Eastern Anatolia, consists of a rhyolitic lava flow, rhyolitic dykes, a trachyandesitic lava flow and basaltic trachyandesitic dykes. Existence of mafic enclaves and globules in some of the volcanic rocks, and microtextures in phenocrysts indicate that magma mingling and mixing between andesitic and basaltic melts played an important role in the evolution of the volcanic suite. Major and trace element characteristics of the volcanic rocks are similar to those formed in convergent margin settings.

Петрогенезис ультрамафитов - одна из наиболее важных проблеы современной геологии. Особенно интересны альпинопшные гипербазиты и коматииты, свойства которых с одной стороны рассматривается как индикаторы глантийных процессов, а с другой - во многого определяют специфические черты металлогении в районах своего развития.

The title of this book may sound like a topic for science fiction, but perhaps even more remarkable is the realization that the information presented here is the result of decadesof detailed scientific studies of the geology of Mars from multiple spacecraft missions.

Key moments in European history can be identified with relative ease, whereas periods of formation or disintegration require more lengthy analysis and argument to define their significance. In prehistory, on the other hand, rarely can significant moments be identified, although with the characterisation of broad periods, change, gradual or otherwise, can be described. The essential outlines of the periods discussed in this book are well known; they pivot around one clearly identifiable event, the cataclysmic eruption of the Santorini (Theran) volcano sometime in the late 17th or late 16th century B.C.

Volcanoes have the power to rock our world, from the spectacular and the beautiful to the violent and the deadly. Introducing Volcanology: A Guide to Hot Rocks is a detailed but accessible introduction to volcanoes and their plumbing systems. Aimed at those with an inquisitive interest in volcanoes as well as the more advanced reader, the ten chapters document different aspects of volcanology. All are illustrated with a wide array of photographs and diagrams to accompany the text, and an A–Z of volcanology is included as a glossary. Since the first edition of this book was published in 2011, a lot has happened in the world of volcanoes and in the world of DougalEARTH. I have been lucky to continue travelling globally to see many of the world’s modern and ancient volcanic rocks (the ‘HOT Rocks’ that form the basis of this guide). Since appearing as ‘Dr Volcano’ on BBC television, I have continued to work with various media projects including CBBC series Fierce Earth, a trip down the Grand Canyon in a wooden boat (BBC/Discovery) and a journey to the very edge of China (Discovery Asia), always looking out for the next Earth Science adventure <...>

In the summer of 1963, when a group of Japanese scientists arrived at the aged building of the Hawaiian Volcano Observatory, run by the U. S. Geological Survey, there began a program of cooperation and friendship between American and Japanese volcanologists that continues to the present. The late Professor Takeshi Minakami, a top volcano-physicist long involved in research at various volcanoes, including Asama, then the most active volcano in Japan, led the Japanese group.

Volcanic activity can have a profound effect on the Earth's atmosphere and environment across many spatial and temporal scales. From being the source of most gases in the atmosphere over geologic time scales, to producing climate change, to threatening aviation, volcanic eruptions as well as non-eruptive volcanic gas and particle emissions provide a strong link between the lithosphere and the impact of the atmosphere on human activities.

The Cenozoic volcanism in the Tyrrhenian Sea region shows a very wide range of petrological, geochemical and isotopic compositions, which cover almost entirely the field of igneous rock occurring worldwide. Volcanic activity took place contemporaneously with the opening of the Ligurian-Provenзal and Tyrrhenian Sea basins, and with the formation of the Apennine-Maghrebian chain.

IN 1993, volcanologist Dr. Stanley Williams was standing inside Galeras, an active volcano located in Colombia, South America (Figure 1.1). Steam was rising around him, and gases were escaping from nearby fumeroles. He had tested the gases and heat from the volcano earlier, and had determined that it was safe to go inside the volcano.