Mineralogical Diversity of Ca<sub>2</sub>SiO<sub>4</sub>-Bearing Combustion Metamorphic Rocks in the Hatrurim Basin: Implications for Storage and Partitioning of Elements in Oil Shale Clinkering

This is the first attempt to provide a general mineralogical and geochemical survey of natural Ca<sub>2</sub>SiO<sub>4</sub>-bearing combustion metamorphic (CM) rocks produced by annealing and decarbonation of bioproductive Maastrichtian oil shales in the Hatrurim Basin (Nege...

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Main Authors: Ella V. Sokol, Svetlana N. Kokh, Victor V. Sharygin, Victoria A. Danilovsky, Yurii V. Seryotkin, Ruslan Liferovich, Anna S. Deviatiiarova, Elena N. Nigmatulina, Nikolay S. Karmanov
Format: Article
Language:English
Published: MDPI AG 2019-07-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/9/8/465
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spelling doaj-4735a80a55b640aca370e5f5eed1da712020-11-24T21:29:15ZengMDPI AGMinerals2075-163X2019-07-019846510.3390/min9080465min9080465Mineralogical Diversity of Ca<sub>2</sub>SiO<sub>4</sub>-Bearing Combustion Metamorphic Rocks in the Hatrurim Basin: Implications for Storage and Partitioning of Elements in Oil Shale ClinkeringElla V. Sokol0Svetlana N. Kokh1Victor V. Sharygin2Victoria A. Danilovsky3Yurii V. Seryotkin4Ruslan Liferovich5Anna S. Deviatiiarova6Elena N. Nigmatulina7Nikolay S. Karmanov8V.S. Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences, 3 Koptyug Avenue, Novosibirsk 630090, RussiaV.S. Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences, 3 Koptyug Avenue, Novosibirsk 630090, RussiaV.S. Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences, 3 Koptyug Avenue, Novosibirsk 630090, RussiaV.S. Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences, 3 Koptyug Avenue, Novosibirsk 630090, RussiaV.S. Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences, 3 Koptyug Avenue, Novosibirsk 630090, RussiaMAPEI Corporation, 1144 E Newport Center Dr, Deerfield Beach, FL 33442, USAV.S. Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences, 3 Koptyug Avenue, Novosibirsk 630090, RussiaV.S. Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences, 3 Koptyug Avenue, Novosibirsk 630090, RussiaV.S. Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences, 3 Koptyug Avenue, Novosibirsk 630090, RussiaThis is the first attempt to provide a general mineralogical and geochemical survey of natural Ca<sub>2</sub>SiO<sub>4</sub>-bearing combustion metamorphic (CM) rocks produced by annealing and decarbonation of bioproductive Maastrichtian oil shales in the Hatrurim Basin (Negev Desert, Israel). We present a synthesis of data collected for fifteen years on thirty nine minerals existing as fairly large grains suitable for analytical examination. The Hatrurim Ca<sub>2</sub>SiO<sub>4</sub>-bearing CM rocks, which are natural analogs of industrial cement clinker, have been studied comprehensively, with a focus on several key issues: major- and trace-element compositions of the rocks and their sedimentary precursors; mineral chemistry of rock-forming phases; accessory mineralogy; incorporation of heavy metals and other trace elements into different phases of clinker-like natural assemblages; role of trace elements in stabilization/destabilization of Ca<sub>2</sub>SiO<sub>4</sub> polymorphic modifications; mineralogical diversity of Ca<sub>2</sub>SiO<sub>4</sub>-bearing CM rocks and trace element partitioning during high-temperature–low-pressure anhydrous sintering. The reported results have implications for mineral formation and element partitioning during high-temperature–low-pressure combustion metamorphism of trace element-loaded bituminous marine chalky sediments (“oil shales”) as well as for the joint effect of multiple elements on the properties and hydration behavior of crystalline phases in industrial cement clinkers.https://www.mdpi.com/2075-163X/9/8/465cement clinkerCa<sub>2</sub>SiO<sub>4</sub> modificationslarniteflamiteye’elimitemayenitetrace element partitioningthreshold limitscombustion metamorphismHatrurim Formation
collection DOAJ
language English
format Article
sources DOAJ
author Ella V. Sokol
Svetlana N. Kokh
Victor V. Sharygin
Victoria A. Danilovsky
Yurii V. Seryotkin
Ruslan Liferovich
Anna S. Deviatiiarova
Elena N. Nigmatulina
Nikolay S. Karmanov
spellingShingle Ella V. Sokol
Svetlana N. Kokh
Victor V. Sharygin
Victoria A. Danilovsky
Yurii V. Seryotkin
Ruslan Liferovich
Anna S. Deviatiiarova
Elena N. Nigmatulina
Nikolay S. Karmanov
Mineralogical Diversity of Ca<sub>2</sub>SiO<sub>4</sub>-Bearing Combustion Metamorphic Rocks in the Hatrurim Basin: Implications for Storage and Partitioning of Elements in Oil Shale Clinkering
Minerals
cement clinker
Ca<sub>2</sub>SiO<sub>4</sub> modifications
larnite
flamite
ye’elimite
mayenite
trace element partitioning
threshold limits
combustion metamorphism
Hatrurim Formation
author_facet Ella V. Sokol
Svetlana N. Kokh
Victor V. Sharygin
Victoria A. Danilovsky
Yurii V. Seryotkin
Ruslan Liferovich
Anna S. Deviatiiarova
Elena N. Nigmatulina
Nikolay S. Karmanov
author_sort Ella V. Sokol
title Mineralogical Diversity of Ca<sub>2</sub>SiO<sub>4</sub>-Bearing Combustion Metamorphic Rocks in the Hatrurim Basin: Implications for Storage and Partitioning of Elements in Oil Shale Clinkering
title_short Mineralogical Diversity of Ca<sub>2</sub>SiO<sub>4</sub>-Bearing Combustion Metamorphic Rocks in the Hatrurim Basin: Implications for Storage and Partitioning of Elements in Oil Shale Clinkering
title_full Mineralogical Diversity of Ca<sub>2</sub>SiO<sub>4</sub>-Bearing Combustion Metamorphic Rocks in the Hatrurim Basin: Implications for Storage and Partitioning of Elements in Oil Shale Clinkering
title_fullStr Mineralogical Diversity of Ca<sub>2</sub>SiO<sub>4</sub>-Bearing Combustion Metamorphic Rocks in the Hatrurim Basin: Implications for Storage and Partitioning of Elements in Oil Shale Clinkering
title_full_unstemmed Mineralogical Diversity of Ca<sub>2</sub>SiO<sub>4</sub>-Bearing Combustion Metamorphic Rocks in the Hatrurim Basin: Implications for Storage and Partitioning of Elements in Oil Shale Clinkering
title_sort mineralogical diversity of ca<sub>2</sub>sio<sub>4</sub>-bearing combustion metamorphic rocks in the hatrurim basin: implications for storage and partitioning of elements in oil shale clinkering
publisher MDPI AG
series Minerals
issn 2075-163X
publishDate 2019-07-01
description This is the first attempt to provide a general mineralogical and geochemical survey of natural Ca<sub>2</sub>SiO<sub>4</sub>-bearing combustion metamorphic (CM) rocks produced by annealing and decarbonation of bioproductive Maastrichtian oil shales in the Hatrurim Basin (Negev Desert, Israel). We present a synthesis of data collected for fifteen years on thirty nine minerals existing as fairly large grains suitable for analytical examination. The Hatrurim Ca<sub>2</sub>SiO<sub>4</sub>-bearing CM rocks, which are natural analogs of industrial cement clinker, have been studied comprehensively, with a focus on several key issues: major- and trace-element compositions of the rocks and their sedimentary precursors; mineral chemistry of rock-forming phases; accessory mineralogy; incorporation of heavy metals and other trace elements into different phases of clinker-like natural assemblages; role of trace elements in stabilization/destabilization of Ca<sub>2</sub>SiO<sub>4</sub> polymorphic modifications; mineralogical diversity of Ca<sub>2</sub>SiO<sub>4</sub>-bearing CM rocks and trace element partitioning during high-temperature–low-pressure anhydrous sintering. The reported results have implications for mineral formation and element partitioning during high-temperature–low-pressure combustion metamorphism of trace element-loaded bituminous marine chalky sediments (“oil shales”) as well as for the joint effect of multiple elements on the properties and hydration behavior of crystalline phases in industrial cement clinkers.
topic cement clinker
Ca<sub>2</sub>SiO<sub>4</sub> modifications
larnite
flamite
ye’elimite
mayenite
trace element partitioning
threshold limits
combustion metamorphism
Hatrurim Formation
url https://www.mdpi.com/2075-163X/9/8/465
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