Titlebook: Merapi Volcano; Geology, Eruptive Ac Ralf Gertisser,Valentin R. Troll,Antonius Ratdomop Book 2023 Springer Nature Switzerland AG 2023 Pyroc

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Physical Environment and Human Context at Merapi Volcano: A Complex Balance Between Accessing Livel publication by the Volcanological Survey of Indonesia in 1978, the danger map has been updated twice, in 2002 and after the deadly eruption of Merapi in 2010. Most of the information is provided by scientists during the ‘raising awareness program’ phase and achieved in the framework of a Community-

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Crustal Structure and Ascent of Fluids and Melts Beneath Merapi: Insights From Geophysical Investigthods different crustal zones could be identified with low-velocity values and high Vp/Vs ratios, which can be explained as fluid- and melt-hosting zones. Large-scale joint seismic experiments (MERAPI, MERAMEX and DOMERAPI) displayed seismic attenuation and scattering effects seen in the shallow por

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The Godean Debris Avalanche Deposit From a Sector Collapse of Merapi Volcano, until the confluence of the Bedog River and the Progo River. In its original form, the Godean debris avalanche flowed 50?km away from Merapi and covered an area of?~390?km.. The gigantic landslide destroyed areas of the Magelang District, Central Java Province, as well as the Sleman, Bantul and the

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The Magma Plumbing System of Merapi: The Petrological Perspective,onally variable magmas within the Merapi plumbing system. Holocrystalline plutonic inclusions comprise gabbro to diorite compositions and are generally coarse grained with occasional mineral layering. Mineral and isotope compositions of the plutonic inclusions largely overlap with those of recent Me

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A Textural Perspective on the Magmatic System and Eruptive Behaviour of Merapi Volcano,losive eruptive behaviour. For example, microlite textures from different stages of the 2010 eruption show that transitions between explosive and effusive activity in 2010 were driven primarily by the dynamics of magma ascent in the shallow conduit.

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Magma-Carbonate Interaction at Merapi Volcano, Indonesia,–O–H gas phase, which may at times place additional pressure on the magmatic system. The detection of extremely low δ.C values in remnant calcite in Merapi xenoliths relative to unmetamorphosed limestone underscores the efficiency of carbonate and calc-silicate degassing during carbonate assimilatio

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Merapi Volcano: From Volcanic Gases to Magma Degassing,as changes precursory to major eruptive events (e.g. the 2010 Plinian eruption). Moreover, the initial abundances and pressure-related behavior of volatile components in Merapi magma were determined from both microprobe analysis of natural samples (melt inclusions, crystal zoning) and petrologic exp