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Chemical Weathering of New Pyroclastic Deposits from Mt. Merapi (Java), Indonesia
by
Dian Fiantis Malik Nelson Eric Van Ranst Jusop Shamshuddin Nikolla P. Qafoku
in
X射线荧光
/ 化学风化
/ 单斜辉石
/ 印度尼西亚
/ 指数和
/ 火山爆发
/ 火山碎屑
/ 碎屑沉积
2009
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Chemical Weathering of New Pyroclastic Deposits from Mt. Merapi (Java), Indonesia
by
Dian Fiantis Malik Nelson Eric Van Ranst Jusop Shamshuddin Nikolla P. Qafoku
in
X射线荧光
/ 化学风化
/ 单斜辉石
/ 印度尼西亚
/ 指数和
/ 火山爆发
/ 火山碎屑
/ 碎屑沉积
2009
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Chemical Weathering of New Pyroclastic Deposits from Mt. Merapi (Java), Indonesia
Journal Article
Chemical Weathering of New Pyroclastic Deposits from Mt. Merapi (Java), Indonesia
2009
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Overview
The Java Island, Indonesia with abundant amount of pyroclastic deposits is located in the very active and dynamic Pacific Ring of Fires. Studying the geochemical weathering indices of these pyroclastic deposits is important to get a clear picture about weathering profiles on deposits resulting from the eruption of Mt. Merapi. Immediately after the first phase of the eruption (March to June 2006), moist and leached pyroclastic deposits were collected. These pyroclastic deposits were found to be composed of volcanic glass, plagioclase feldspar in various propoitions, orthopyroxene, clinopyroxene, olivine, amphibole and titanomagnetite. The total elemental composition of the bulk samples (including trace elements and heavy metals) was determined by wet chemical methods and X-ray fluorescence (XRF) analyses. Weathering of the pyroelastic deposits was studied using various weathering indices. The Ruxton ratio, weathering index of Parker, Vought resudual index and chemical index of weathering of moist pyroclastic deposits were lower than those of the leached samples, but the alteration indices (chemical and plagioclase) were slightly higher in the moist compared to the leached pyroelastic deposits.
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