Search for Articles:
Title / Keyword
Author / Affiliation / Email
Journal
Article Type
 
 
Advanced Search
 
Section
Special Issue
Volume
Issue
Number
Page
 
4.1
2.2
Journals
Minerals
Special Issues
Mineral Formation in Pyrometamorphic Process
share announcement

Mineral Formation in Pyrometamorphic Process

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Geochemistry and Geochronology".

Deadline for manuscript submissions: closed (15 September 2020) | Viewed by 19347

Special Issue Editors

Dr. Victor V. Sharygin

E-Mail Website
Guest Editor
V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the RAS, 630090 Novosibirsk, Russia
Interests: pyrometamorphism; combustion metamorphism; coal fires; burned dumps; paralava; new minerals; silicate-melt and fluid inclusions in minerals; mineralogy of alkaline rocks; carbonatites; kimberlites; mineralogy of meteorites
Special Issues, Collections and Topics in MDPI journals
Dr. Ellina V. Sokol

E-Mail Website
Guest Editor
V.S.Sobolev Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences, Novosibirsk, Russia
Interests: pyrometamorphism; combustion metamorphism; unhydrous melted rocks; coal fires; burned dumps; new minerals; cement mineralogy; mineralogical diversity; mud volcanism; geochemistry
Prof. Dr. Rodney Grapes

E-Mail
Guest Editor
School of Earth Science and Engineering, Sun Yat-sen University, Guangzhou 510275, China
Interests: pyrometamorphism; combustion metamorphism; metamorphic petrology; mineralogy and geochemistry

Special Issue Information

Dear Colleagues,

Pyrometamorphism is a common phenomenon in the Earth’s history and involves all stages of transformation of rocks (typically sediments) into high-temperature mineral associations (up to the melting stage) and their subsequent retrograde alteration under near-surface conditions. The pyrometamorphic process is very similar in both natural and anthropogenic environments.

Pyrometamorphic rocks include xenoliths of various compositions in mafic volcanic/plutonic rocks, wall rocks of mafic magma intrusion/extrusion, and sedimentary rocks that have been heated by the combustion of coal and other caustobiolith strata, flame burning in mud volcanoes, etc. Such high-temperature/low pressure transformation of sedimentary protoliths may lead to high mineral diversity, which strongly depends on the initial composition of the rocks, heating temperature, redox conditions, and other factors. For example, more than 200 minerals have been found in the unique Hatrurim Formation (Israel–Jordan), and some of them indicate very specific pyrometamorphic conditions.

This Special Issue invites contributions dealing with mineralogical and petrographic aspects in pyrometamorphic processes: the discovery of new minerals, the chemistry and geochemistry of minerals and rocks, the melting and formation of paralavas, the mineralogy of retrograde associations, fumarole mineralization in burned complexes, etc. Papers concerning the mineralogy of technogenic combustion (burned dumps of coal mines, catastrophic man-induced fires, industrial microspheres, burning of waste material, etc.) are also welcome.

The aim of this Special Issue is to collect research papers devoted to recent studies of the mineralogy and petrology of pyrometamorphic rocks.

Dr. Victor V. Sharygin
Dr. Ellina V. Sokol
Prof. Dr. Rodney Grapes
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Minerals is an international peer-reviewed open access monthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2400 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • Xenoliths in igneous rocks and contact metamorphism
  • Mineralogy and petrography of pyrometamorphic complexes
  • Hatrurim formation
  • Burning in mud volcanoes
  • Minerals and rocks in natural coal fires
  • Burned coal dumps
  • Fumarole mineralization during combustion metamorphism
  • New, endemic, and rare pyrometamorphic minerals
  • Silicate-melt and fluid inclusions in pyrometamorphic minerals

Benefits of Publishing in a Special Issue

  • Ease of navigation: Grouping papers by topic helps scholars navigate broad scope journals more efficiently.
  • Greater discoverability: Special Issues support the reach and impact of scientific research. Articles in Special Issues are more discoverable and cited more frequently.
  • Expansion of research network: Special Issues facilitate connections among authors, fostering scientific collaborations.
  • External promotion: Articles in Special Issues are often promoted through the journal's social media, increasing their visibility.
  • e-Book format: Special Issues with more than 10 articles can be published as dedicated e-books, ensuring wide and rapid dissemination.

Further information on MDPI's Special Issue polices can be found here.

Published Papers (5 papers)

Download All Papers
Order results
Result details
Show export options expand_more Show export options expand_less
Select all
Export citation of selected articles as:

Research

22 pages, 14474 KiB  
Article
Petrography, Mineralogy, and Geochemistry of Combustion Metamorphic Rocks in the Northeastern Ordos Basin, China: Implications for the Origin of “White Sandstone”
by Bin Chen, Yanyan Wang, Marco Franceschi, Xiong Duan, Kuizhou Li, Yu Yu, Meiling Wang and Zhiqiang Shi
Minerals 2020, 10(12), 1086; https://doi.org/10.3390/min10121086 - 3 Dec 2020
Cited by 8 | Viewed by 3251
Abstract
Since the Quaternary period, tectonic uplift and river erosion in the northeastern Ordos Basin (northwest China) have exhumed numerous coal seams, creating the conditions for the development of coal fires following their spontaneous combustion or other types of ignition (e.g., lightning strikes). Coal [...] Read more.
Since the Quaternary period, tectonic uplift and river erosion in the northeastern Ordos Basin (northwest China) have exhumed numerous coal seams, creating the conditions for the development of coal fires following their spontaneous combustion or other types of ignition (e.g., lightning strikes). Coal fires activity is testified by the widespread occurrence of combustion metamorphic rocks. In this study, thin section analyses, scanning electron microscopy, X-ray diffraction (XRD), X-ray fluorescence (XRF), and inductively coupled plasma mass spectrometry (ICP-MS) were used to investigate in detail the mineralogical and geochemical characteristics of combustion metamorphic rocks in the Jurassic succession of the northeastern Ordos Basin. The samples collected in localities distributed over an area of about 8000 km2 were analyzed to determine their mineral association, revealing the presence of tridymite, cristobalite, mullite, and cordierite that are typically produced in pyrometamorphic reactions. XRF and ICP-MS analyses revealed that combustion metamorphic rocks are iron-enriched. Investigations in the study area also highlighted the occurrence of a peculiar, porous, and permeable white sandstone that appears often associated with clinkers or coal seams. It is composed of quartz and feldspar grains and cemented by kaolinite. It is here suggested that the white color of this sandstone could be due to coal fire-related kaolinization of a sandstone protolith produced by the acidic low-temperature hydrothermal circulation of rain waters during times of coal fire activity. Full article
(This article belongs to the Special Issue Mineral Formation in Pyrometamorphic Process)
►▼ Show Figures

Figure 1

45 pages, 9929 KiB  
Article
Ultrahigh-Temperature Sphalerite from Zn-Cd-Se-Rich Combustion Metamorphic Marbles, Daba Complex, Central Jordan: Paragenesis, Chemistry, and Structure
by Ella V. Sokol, Svetlana N. Kokh, Yurii V. Seryotkin, Anna S. Deviatiiarova, Sergey V. Goryainov, Victor V. Sharygin, Hani N. Khoury, Nikolay S. Karmanov, Victoria A. Danilovsky and Dmitry A. Artemyev
Minerals 2020, 10(9), 822; https://doi.org/10.3390/min10090822 - 17 Sep 2020
Cited by 18 | Viewed by 4382
Abstract
Minerals of the Zn-Cd-S-Se system that formed by moderately reduced ~800–850 °C combustion metamorphic (CM) alteration of marly sediments were found in marbles from central Jordan. Their precursor sediments contain Se- and Ni-enriched authigenic pyrite and ZnS modifications with high Cd enrichment (up [...] Read more.
Minerals of the Zn-Cd-S-Se system that formed by moderately reduced ~800–850 °C combustion metamorphic (CM) alteration of marly sediments were found in marbles from central Jordan. Their precursor sediments contain Se- and Ni-enriched authigenic pyrite and ZnS modifications with high Cd enrichment (up to ~10 wt%) and elevated concentrations of Cu, Sb, Ag, Mo, and Pb. The marbles are composed of calcite, carbonate-fluorapatite, spurrite, and brownmillerite and characterized by high P, Zn, Cd, U, and elevated Se, Ni, V, and Mo contents. Main accessories are either Zn-bearing oxides or sphalerite, greenockite, and Ca-Fe-Ni-Cu-O-S-Se oxychalcogenides. CM alteration lead to compositional homogenization of metamorphic sphalerite, for which trace-element suites become less diverse than in the authigenic ZnS. The CM sphalerites contain up to ~14 wt% Cd and ~6.7 wt% Se but are poor in Fe (means 1.4–2.2 wt%), and bear 100–250 ppm Co, Ni, and Hg. Sphalerite (Zn,Cd,Fe)(S,O,Se)cub is a homogeneous solid solution with a unit cell smaller than in ZnScub as a result of S2− → O2− substitution (a = 5.40852(12) Å, V = 158.211(6) Å3). The amount of lattice-bound oxygen in the CM sphalerite is within the range for synthetic ZnS1−xOx crystals (0 < x ≤ 0.05) growing at 900 °C. Full article
(This article belongs to the Special Issue Mineral Formation in Pyrometamorphic Process)
►▼ Show Figures

Figure 1

23 pages, 5032 KiB  
Article
The Behaviour of Siderite Rocks in an Experimental Imitation of Pyrometamorphic Processes in Coal-Waste Fires: Upper and Lower Silesian Case, Poland
by Łukasz Kruszewski and Justyna Ciesielczuk
Minerals 2020, 10(7), 586; https://doi.org/10.3390/min10070586 - 29 Jun 2020
Cited by 5 | Viewed by 2731
Abstract
Little is known of the influence of fluxes on the nature and the intensity of burning in coal-waste heaps. To gain some insight, two siderite samples, one each from coal-mining waste heaps in Upper- and Lower Silesian Coal Basins (Poland), were heated under [...] Read more.
Little is known of the influence of fluxes on the nature and the intensity of burning in coal-waste heaps. To gain some insight, two siderite samples, one each from coal-mining waste heaps in Upper- and Lower Silesian Coal Basins (Poland), were heated under identical conditions in a thermal chamber coupled to a powder X-ray diffractometer. Differences in the behaviour of siderite phase and the products of its decomposition, mainly magnetite, wüstite, and olivine, are discussed. The waste heaps sampled underwent self-heating and self-ignition catalysed by fluxes. Though the samples are unlikely to be truly representative of the Silesian basins, the heterogeneous behaviour they displayed on heating merits description and explanation, as siderite is an important widely known flux in pyrometamorphic processes. Full article
(This article belongs to the Special Issue Mineral Formation in Pyrometamorphic Process)
►▼ Show Figures

Graphical abstract

24 pages, 9853 KiB  
Article
Pyrometamorphic Rocks in the Molinicos Basin (Betic Cordillera, SE Spain): Insights into the Generation of Cordierite Paralavas
by Isabel Abad, Mario Sánchez-Gómez, Matías Reolid and Vicente López Sánchez-Vizcaíno
Minerals 2019, 9(12), 748; https://doi.org/10.3390/min9120748 - 30 Nov 2019
Cited by 2 | Viewed by 3975
Abstract
A singular thermal anomaly occurred in the Molinicos Miocene, lacustrine, intramontane basin (Betic Cordillera). This gave place to vitreous vesicular materials (paralavas) and baked rocks (clinker) inside of a sequence of marly diatomites and limestones. The chemical composition of the paralavas (SiO2 [...] Read more.
A singular thermal anomaly occurred in the Molinicos Miocene, lacustrine, intramontane basin (Betic Cordillera). This gave place to vitreous vesicular materials (paralavas) and baked rocks (clinker) inside of a sequence of marly diatomites and limestones. The chemical composition of the paralavas (SiO2 = 52–57, Al2O3 ≈ 20, Fe2O3 = 10–20, K2O + Na2O < 2.5, CaO < 4.5, and MgO < 1.5, % in weight), which is very different from typical igneous rocks, and their high-T mineralogy (cordierite, sillimanite, anorthite, mullite, and high-T silica polymorphs) suggest that they formed during a pyrometamorphic event. The occurrence of dry intervals in the lacustrine depositional system, the high Total Organic Carbon contents (>4% in weight) of dark clay layers and the existence of tectonic fractures give the right context for a combustion process. Short-term heating favoured the generation of paralavas, clinker and marbles. Thermodynamic modelling constrains the onset of melting at 870–920 °C for <10 MPa at equilibrium conditions. However, the presence of tridymite and/or cristobalite in clinker and paralavas and the compositional variation in both rock types suggests that the temperature at which first melting occurred ranged between 870 °C and 1260 °C due to melt fractionation processes. Full article
(This article belongs to the Special Issue Mineral Formation in Pyrometamorphic Process)
►▼ Show Figures

Figure 1

26 pages, 6680 KiB  
Article
Nataliakulikite, Ca4Ti2(Fe3+,Fe2+)(Si,Fe3+,Al)O11, a New Perovskite-Supergroup Mineral from Hatrurim Basin, Negev Desert, Israel
by Victor V. Sharygin, Grigory A. Yakovlev, Richard Wirth, Yurii V. Seryotkin, Ellina V. Sokol, Elena N. Nigmatulina, Nikolai S. Karmanov and Leonid A. Pautov
Minerals 2019, 9(11), 700; https://doi.org/10.3390/min9110700 - 13 Nov 2019
Cited by 6 | Viewed by 4075
Abstract
Nataliakulikite, Ca4Ti2(Fe3+,Fe2+)(Si,Fe3+,Al)O11, is a mineral intermediate between perovskite CaTiO3 and brownmillerite Ca2(Fe,Al)2O5. It was discovered as a minor mineral in a high-temperature pyrometamorphic larnite-gehlenite [...] Read more.
Nataliakulikite, Ca4Ti2(Fe3+,Fe2+)(Si,Fe3+,Al)O11, is a mineral intermediate between perovskite CaTiO3 and brownmillerite Ca2(Fe,Al)2O5. It was discovered as a minor mineral in a high-temperature pyrometamorphic larnite-gehlenite rock at the Nahal Morag Canyon of the Hatrurim Basin, Israel. Nataliakulikite is associated with larnite, flamite, gehlenite, magnesioferrite, Fe3+-rich perovskite, fluorapatite, barite, Hashemite, and retrograde phases (afwillite, hillebrandite, portlandite, calcite, ettringite, hydrogarnet, and other hydrated Ca-silicates). The mineral forms brown subhedral or prismatic grains (up to 20 µm) and their intergrowths (up to 50 μm). Its empirical formula (n = 47) is (Ca3.992Sr0.014U0.004)(Ti1.933Zr0.030Nb0.002) (Fe3+0.610Fe2+0.405Cr0.005Mn0.005)(Si0.447Fe3+0.337Al0.216)O11 and shows Si predominance in tetrahedral site. The unit-cell parameters (HRTEM data) and space group are: a = 5.254, b = 30.302, c = 5.488 Å, V = 873.7 Å3, Pnma, Z = 4. These dimensions and Electron backscatter diffraction (EBSD) data strongly support the structural identity between nataliakulikite and synthetic Ca4Ti2Fe3+2O11 (2CaTiO3∙Ca2Fe3+2O5), an intermediate compound in the system CaTiO3-Ca2Fe3+2O5. In general, this mineral is a Si-Fe2+-rich natural analog of synthetic Ca4Ti2Fe3+2O11. The X-ray powder diffraction data (CuKα -radiation), calculated from unit-cell dimensions, show the strongest lines {d [Å], (Icalc)} at: 2.681(100), 1.898(30), 2.627(26), 2.744(23), 1.894(22), 15.151(19), 1.572(14), 3.795(8). The calculated density is 4.006 g/cm3. The crystal structure of nataliakulikite has not been refined because of small sizes of grains. The Raman spectrum shows strong bands at 128, 223, 274, 562, and 790 cm−1. Nataliakulikite from the Hatrurim Basin crystallized under the conditions of combustion metamorphism at high temperatures (1160–1200 °C) and low pressures (HT-region of the spurrite-merwinite facies). Full article
(This article belongs to the Special Issue Mineral Formation in Pyrometamorphic Process)
►▼ Show Figures

Figure 1

Show export options expand_more Show export options expand_less
Select all
Export citation of selected articles as:
 
Displaying articles 1-5
Back to TopTop