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Crystal structure and crystal chemis...

Uvarova, Yulia A.

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Crystal structure and crystal chemistry of amphiboles in the Kola Superdeep Borehole section as related to lithology, metamorphic grade and environment of Precambrian rocks.

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
正題名/作者:	Crystal structure and crystal chemistry of amphiboles in the Kola Superdeep Borehole section as related to lithology, metamorphic grade and environment of Precambrian rocks./
作者:	Uvarova, Yulia A.
面頁冊數:	424 p.
附註:	Source: Dissertation Abstracts International, Volume: 70-08, Section: B, page: 4713.
Contained By:	Dissertation Abstracts International70-08B.
標題:	Geology. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=NR50457
ISBN:	9780494504574

Crystal structure and crystal chemistry of amphiboles in the Kola Superdeep Borehole section as related to lithology, metamorphic grade and environment of Precambrian rocks.
Uvarova, Yulia A.

Crystal structure and crystal chemistry of amphiboles in the Kola Superdeep Borehole section as related to lithology, metamorphic grade and environment of Precambrian rocks. - 424 p.

Source: Dissertation Abstracts International, Volume: 70-08, Section: B, page: 4713.

Thesis (Ph.D.)--University of Manitoba (Canada), 2008.

The Kola Superdeep Borehole (KSDB) is a continuous 12.2 km section of crust that crosses the Proterozoic-Archean boundary and two major thrust systems, the Luchlompol fault and the Titovsko-Ambarnyi fault. The mineral assemblages from approximately 120 samples from the core of the Kola Superdeep Borehole and their surface analogues have been examined by a wide range of techniques: single-crystal X-ray diffraction, single-crystal and powder milli-Mossbauer spectroscopy, electron-microprobe analysis, inductively-coupled plasma optical emission spectroscopy, inductively-coupled plasma mass spectrometry, optical petrography and stable-isotope analysis for oxygen and hydrogen. As a result of using such a wide variety of analytical technique, the analytical data and site populations of the studied amphiboles are of much higher accuracy than is usually the case for petrological studies of metamorphic rocks.

ISBN: 9780494504574Subjects--Topical Terms:

516570
Geology.

Crystal structure and crystal chemistry of amphiboles in the Kola Superdeep Borehole section as related to lithology, metamorphic grade and environment of Precambrian rocks.
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245 1 0 $a Crystal structure and crystal chemistry of amphiboles in the Kola Superdeep Borehole section as related to lithology, metamorphic grade and environment of Precambrian rocks.
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500 $a Source: Dissertation Abstracts International, Volume: 70-08, Section: B, page: 4713.
502 $a Thesis (Ph.D.)--University of Manitoba (Canada), 2008.
520 $a The Kola Superdeep Borehole (KSDB) is a continuous 12.2 km section of crust that crosses the Proterozoic-Archean boundary and two major thrust systems, the Luchlompol fault and the Titovsko-Ambarnyi fault. The mineral assemblages from approximately 120 samples from the core of the Kola Superdeep Borehole and their surface analogues have been examined by a wide range of techniques: single-crystal X-ray diffraction, single-crystal and powder milli-Mossbauer spectroscopy, electron-microprobe analysis, inductively-coupled plasma optical emission spectroscopy, inductively-coupled plasma mass spectrometry, optical petrography and stable-isotope analysis for oxygen and hydrogen. As a result of using such a wide variety of analytical technique, the analytical data and site populations of the studied amphiboles are of much higher accuracy than is usually the case for petrological studies of metamorphic rocks.
520 $a Chemical composition and site-populations of KSDB amphiboles were related to metamorphic grade, relative depth in the borehole and P-T conditions in KSDB rocks and bulk-rock chemistry. Chemical compositions of co-existing amphibole and plagioclase were used to calculate temperatures and pressures of prograde metamorphism; chemical composition of chlorite was used to calculate the temperature of retrograde metamorphism that affected Kola Superdeep Borehole rocks.
520 $a Variable chemical components in co-existing calcic amphibole, plagioclase, biotite and titanite show monotonic relations with the relative depth in the borehole and metamorphic grade. This indicates that the variation in depth in the borehole reflects a real change in metamorphic grade, and that there is no major tectonic hiatus disturbing the gradual increase in metamorphic grade with the depth in the borehole.
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