On the origin and morphology of Z-shaped splitting of coal deposits (on the example of Eastern Donbass)

Статья посвящена выявлению морфологии и происхождения распространенных во многих угольных регионах мира уникальных углепородных структур – Z-образных расщеплений угольных залежей, впервые обнаруженных автором в Восточном Донбассе. Актуальность работыопределяется необходимостью разработки научных основ угленакопления для определения промышленной ценности и минерагенических перспектив территорий. Цель работы. Совершенствование теории угленакопления и первичного структурообразования в осадочных формациях в целом. Методы работы. Вещественно-структурный анализ пересекающихся геологических разрезов угленосной территории западной части Восточного Донбасса известными литолого-структурными методами, сопоставление выявленного Z-объекта с аналогичными структурами других угольных регионов и гипотез о формировании Z-расщеплений. Результаты работы. Обнаружено и исследовано первое в Восточном Донбассе Z-образное расщепление угольной залежи. Залежь k2н каменской свиты С25 каменноугольной системы у г. Красный Сулин асимметрична в разрезе и плане. Высота Z-объекта составляет первые десятки метров, площадь – многие десятки км2, протяженность с севера на юг превышает 20 км. Объект имеет угольные основание и свод в плане, сопряжение их угольным соединением. Z-образность объекта проявляется в субмеридиональных сечениях. Уникальны односторонняя – с запада – замкнутость соединения, наличие угольных пачек-перемычек, неразвившихся до соединения. Выявлена этапность формирования объекта. На конкретном примере определены условия развития Z-объектов: попеременное фронтальное поступление крупных сбалансированных порций в основном растительного или растительно-минерального материала на смежные участки территории с разных сторон с частичным заходом языка минеральных осадков на покрытый углематеринской массой один из них. Нарушение условий приводит к отклонению облика структуры от типовой либо прекращению ее образования. Механизм поступления материала – разливы рукавов палеодельты. Односторонняя замкнутость соединения в плане вызвана поступлением локальных потоков минерального материала. Ниша седиментации создана процессами тектонического относительного опускания смежных участков территории. Исследованная структура возникла в условиях сочетания тектонических и седиментационных предпосылок, главный вклад в ее формирование принадлежит деятельности палеорусел. В этой связи структура отнесена к аккумулятивному типу. Приведены примеры других Z-объектов. Z-структуры развиты на различных масштабных уровнях. Результаты исследований имеют значение для различных регионов угленакопления и решения общих вопросов седиментации. The article is dedicated to the identification of the morphology and origin of unique coal-bearing structures common in many coal regions of the world - Z-shaped splitting of coal deposits, first discovered by the author in the Eastern Donbass. The relevance of the work is determined by the need to develop the scientific foundations of coal accumulation to determine the industrial value and mineragenic prospects of the territories. Aim. Improvement of the theory of coal accumulation and primary structure formation in sedimentary formations in general. Methods. Material-structural analysis of intersecting geological sections of the coal-bearing territory of the western part of the Eastern Donbass using well-known lithological-structural methods, comparison of the identified Z-object with similar structures of other coal regions and hypotheses about the formation of Z-splits. Results. The first Z-shaped splitting of a coal deposit in the Eastern Donbas was discovered and investigated. The k2n deposit of the Kamenskaya suite C25 of the Carboniferous system near the town of Krasny Sulin is asymmetric in section and plan. The height of the Z-object is the first tens of meters, the area is many tens of km2, and the length from north to south is 20 km wide. The object has a coal base and a vault in plan, their conjugation with a carbon connection. The Z-shape of the object appears in submeridional sections. Unique is the one-sided - from the west - closed connection, the presence of coal bundles-bridges that did not develop before the connection. The stages in the formation of the object are revealed. On a specific example of the conditions for the development of Z-objects: the transverse frontal supply of large balanced portions of mainly plant or plant-mineral material in different parts of the territory from different mineral sediments with a partial entry of the tongue onto one of them covered with a source coal mass. Violation of the conditions leads to a deviation of the structure from the typical one or to the termination of its formation. The mechanism of material receipt is the spill of the paleodelta arms. One-sided closedness of the connection is in terms of providing local flows of mineral material. The sedimentation niche was created by the processes of tectonic relative subsidence of additional areas of the territory. The investigated structure arose under the conditions of a combination of tectonic and sedimentation prerequisites; the main contribution to its formation was the activity of the paleochannels. In this regard, the structure is classified as an accumulative type. Examples of other Z - objects are given. Z-structures are developed at various levels. Research results are of significance for different regions of coal accumulation and solution of general sedimentation issues.

The Burial Under Peat Technique: An Innovative Method to Restore Sphagnum Peatlands Impacted by Mineral Linear Disturbances

Mineral roads in peatlands change the nature of the substrate, influence the water table level of the peatland on either side of the road and the physicochemical characteristics of the water and peat. These changes can in turn affect plant community composition. The efficiency of an innovative and affordable method for the restoration of peatlands impacted by roads was evaluated: the Burial Under Peat Technique. To be considered effective from an ecological point of view, the technique should meet restoration goals by 1) confining the chemical elements and compounds potentially leaching from the mineral material; 2) creating and maintaining a restored surface elevation similar to the adjacent peatland for optimal rewetting; and 3) re-establishing typical peatland vegetation communities. Three years post-restoration, water sampled at various depths and distances to the buried road presented chemical elements and compounds concentrations similar to the means measured in the pristine surrounding peatland for most of the ions analyzed. The different steps of the technique ensured the reestablishment of an elevation similar to the surrounding peatland. The return of peatland plant communities was slow, mainly due to local factors (e.g., presence of drainage ditches). Furthermore, the Burial Under Peat Technique fulfilled the restoration objectives in re-establishing an acid organic soil. Finally, it is a cost-effective method in comparison to completely removing the mineral material and transporting new material to fill the depression left by the excavation of the road.

Analisis Kandungan Mineral Pasir Pantai Bajul Mati Kabupaten Malang Menggunakan XRF dan XRD

Mineral exploration in Indonesia has not been evenly distributed, so a study with title analysis of the sand mineral content of Bajul Mati Malang Regency was carried out using XRF and XRD. The aims of this study to determine the percentage of mineral that containing in the sand of Bajul Mati beach in Malang Regency. The instruments used XRF and XRD where the samples were placed in a sample holder and irradiated with X-rays then. The result of analysis of mineral content and metal oxide in Bajul Mati beach sand showed that the beach sand of Bajul Mati has the big potential to be used as a base for making nanomaterials. The results of analysis of XRF showed that the content of SiO2 was 46.7% and the results of analysis of XRD showed that the SiO2 mineral has the quartz phased. Bajul Mati beach sand has the potential to be a source of mineral material.

Comparative experiments on the activation cyanide and chloride re-leaching of gold from the secondary mineral material of heaps of Aprelkovo mine

This article presents the results of comparative experiments on the activation chloride and activation carbonate-cyanide leaching of gold from the secondary mineral material of heaps of Aprelkovo mine. A cyanide scheme with a gradual increase in the cyanide concentration in the pregnant solution was adopted as a control scheme for percolation leaching. To establish the maximum recovery of gold and associated components, preliminary experiments with agitational cyanide leaching were carried out. In the course of the experimental work, some of the problems of gold recovery according to the classical cyanide scheme applicable to this deposit were identified and, thanks to the use of activated solutions, were solved. The reasons for the insufficiently high recovery are clogging and limited access of the complexing agent to encapsulated and chemically bound gold inclusions due to their high dispersion in the crystal lattices of concentrating minerals and the presence in the ore of minerals that tend to absorb water with a pronounced hydration effect.