Minerals In Recent Sediments Research Articles

Distribution pattern of heavy minerals assemblages in recent sediments of Lesser Zab River Basin (LZRB), NE Iraq

The Lesser Zab River (LZR), the largest tributary in Iraq, with a catchment area of about 20,000 km2, and majority of its basin lying in Iraq, drains into the Tigris River. It runs through highly folded and faulted igneous and metamorphic zone in the northeastern part of Iraq. We studied the heavy minerals in recent sediments of the Lesser Zab River Basin (LZRB) to determine their mineralogies, assemblages pattern, distribution manner, spatial variability, microtexture, provenance, and tectonic setting. We analyzed 24 sediment samples for heavy mineral assemblage determination, using the standard petrographic method. Scanning Electron Microscopy was used to determine the morphology of the grains of selected heavy minerals. Heavy minerals identified in the studied sediments include: dark color such as magnetite, ilmenite, hematite, and goethite; and transparent minerals represented by hornblende, tremolite–actinolite; pyroxenes, epidotes, zircon, tourmaline, rutile, garnet, staurolite, kyanite, and layered minerals assemblage such as muscovite, chlorite, biotite, and phlogopite. The studied sediments are considered immature, because they have the lowest concentration of ultrastable minerals compared to unstable heavy minerals, which confirms that the surface sediments of LZR and its sub-basin tributaries were deposited in an active continental-margin tectonic setting.

Clay-mineral and grain-size distributions in surface sediments of the White Sea (Arctic Ocean): indicators of sediment sources and transport processes

In this study, the grain-size and clay-mineral compositions of 73 surface sediment samples collected in a variety of environmental settings in the White Sea are presented to characterize recent sedimentation processes, reconstruct transport pathways, and identify potential source areas of the terrigenous components. Areas >100 m deep are invariably characterized by silty clay, whereas areas <100 m deep exhibit more heterogeneous grain-size compositions plausibly explained by coastal erosion and (re-)distribution mechanisms, particularly tidal currents. The dominance of sand in the estuarine areas of the Onega and Dvina rivers as well as toward the Gorlo Strait connecting the White Sea with the Barents Sea is attributed to increased current speeds. Illite and smectite are the dominant clay minerals in recent sediments of the southwestern and eastern White Sea sectors, respectively. Their distribution patterns largely depend on the geology of the source areas, and mirror surface circulation patterns, especially in Dvina Bay. Smectite is a key clay mineral in White Sea surface sediments, as it reveals the dominating influence of the Northern Dvina’s runoff on sedimentation and water circulation throughout the basin. In comparison to other Eurasian shelf seas, the White Sea is characterized by a greater diversity of clay-mineral assemblages, which range from illite- to smectite-dominated sectors containing variable amounts of chlorite and kaolinite.

Clay minerals in recent sediments of the World Ocean and their relation to types of lithogenesis

Problem of the distribution of clay minerals in water areas of the World Ocean and their relation to different (humid, arid, and volcanosedimentary) types of lithogenesis is considered. It is shown that layer silicates can be used as index minerals for distinguishing types of lithogenesis under conditions of marine sedimentation. Humid marine lithogenesis is represented by sediments of the White, Baltic, Black, and Mediterranean seas. Genetic link of marine clay formation with soil-climatic zones is clearly manifested in recent sediments of the World Ocean. Accumulation of statistic data on the mineral composition of clays allowed us to distinguish two modes of spatial-latitudinal distribution of clay minerals: maximal concentrations of illites and chlorites are confined to high latitudes, whereas kaolinite and smectite accumulate in the equatorial zone. In the arid lithogenesis, the dependence of clay formation on drainage areas is practically absent. The whole process is realized in surficial sediments and bottom waters: under conditions of intense evaporation, especially in closed water basins, the concentration of elements in the medium is enough for the synthesis of layer silicates, such as palygorskite and sepiolite. The processes were studied based on the Paleogene Fergana Bay and bottom sediments of the Sea of Aral, as well as DSDP core materials from the Atlantic (near the western coast of Africa) and Indian (the Arabian Peninsula area) oceans. The investigation of processes of volcanosedimentary lithogenesis was carried out within the East Pacific Rise (on the basis of core materials obtained during cruises of R/V Dmitry Mendeleev and Akademik Kurchatov). The results obtained made it possible to establish authigenic (primarily celadonite) K-Fe mineralization in the most active geothermal zones. The formation of clay minerals has specific features in each of the studied (humid, arid, and volcanosedimentary) types of lithogenesis. This should be taken into consideration during the lithological investigations and the study of clay mineralogy of past geological epochs. Clay minerals (particularly, unstable mixed-layered phases) are actively used as index minerals for paleogeographic and climatologic reconstructions.

Clay Minerals in Sediments of the Arctic Seas

The distribution of clay minerals in recent sediments on the Arctic shelf off the Eurasian and North American continents is considered. Prominence is given to the East Siberian and Laptev seas. The illite belt established on the basis of the composition of clay minerals in seven Arctic seas stretches from the Beaufort Sea to the White Sea and reveals a mineralogical zonality. The belt can be devided into smectite and chlorite provinces. Factors governing the formation of the Arctic illite belt and features of the distribution of individual clay minerals are discussed. The identification of the illite belt in sediments on the Arctic shelf complements the system of planetary latitudinal zones of clay minerals formulated by previous researchers.

Clay minerals in recent sediments of the continental shelf and the Bay of Cádiz (SW Spain)

AbstractThe distribution of clay minerals in recent sediments on the continental shelf and in the Bay of Cádiz has been analysed as part of a wider study of sedimentary exchange between the continent and the continental margin. The clay minerals included in the muddy sediments consist mainly of illite, kaolinite, smectite, randomly mixed-layered illite-smectite, chlorite, vermiculite and randomly mixed-layered illite-chlorite. Distribution of the minerals indicates that inheritance from the adjacent continental areas is the most important process involved.The relations between the clay minerals were established by Q-mode and R-mode factor analysis. The main clay mineral associations are: (1) illite-kaolinite, (2) smectite-random mixed-layered illitesmectite, and (3) kaolinite-random mixed-layered illite-smectite-vermiculite. The main sources of sediment supply to the continental shelf are the Guadalquivir and Guadiana rivers. Sediment from these rivers and from the rivers flowing into the Bay of Cádiz (mainly the Guadalete) is transported to the part of the shelf outside the bay by ebb-tide currents. The path of this outflow to the continental shelf, where the sediment is partially deposited, is influenced by the morphology of the coast and by hydrodynamic processes.

The distribution of clay minerals in recent sediments of the Korea Strait

The bottom sediments of the Korea Strait contain, on average, 50% illite, 21% kaolinite, 17% intergrade clay, 8% chlorite, and 4% smectite. The geographical distribution of the clay minerals shows an increase in illite, a decrease in kaolinite and a slight decrease in chlorite seawards. The distributional patterns of smectite and intergrade clay are irregular. The clay fractions of the sediments near the land are supplied by river-borne sediments and are mixed with sediments transported landwards from offshore. The distribution of clay minerals in the Korea Strait appears to have been influenced by the supply or/and redistribution of fine-grained sediments by the Tsushima Warm Current from the East China Sea. Kaolinite seems to be transported mainly by river runoff; and illite, chlorite and smectite might have been derived partly from the East China Sea by the Tsushima Warm Current. Intergrade clay seems to have a complex origin.

The distribution of clay minerals in recent sediments of the Okhotsk Sea

Abstract The clay fractions of surface sediments from the Okhotsk Sea contain montmorillonite, chlorite, illite, and small amounts of kaolinite. The concentrations of these minerals differ from place to place, but they are not determined by submarine topography such as basins and rises. The distribution seems to be influenced mainly by the supply of clay minerals from volcanic materials, various rocks, and soils in the bordering lands.

Clay Distributions in Recent Estuarine Sediments

AbstractThe distribution of clay minerals in Recent sediments can be explained by the relative stability of the clays. The rates of particle aggregation for three clays were determined in the laboratory in synthetic estuarine solutions; from the kinetic studies stability values were calculated. The results indicate that illite is more stable than kaolinite which is more stable than montmorillonite. The distribution of the clays in the Pamlico River Estuary can be explained on the basis of relative clay stability where kaolinite which aggregates rapidly (relatively unstable clay) is found upstream of illite.

Clay Minerals in Recent Sediments of the Niger Delta

AbstractRecent sediments of the Niger delta contain the detrital clay minerals kaolinite, mont-morillonite and a small amount of illite. The montmorillonite content increases with water depth and distance from the shore, and the results of laboratory experiments on natural Niger delta clay support the assumption that this is due to differential floc-culation and sedimentation.The easterly Guinea Current, transporting montmorillonite-rich floccules in suspension, may cause an increase in the montmorillonite content of the clays in the ©cistern part of the delta.Mineralized faecal pellets are present in most marine sediment samples. Chamosite occurs authigenically in coastal water shallower than 35 fathoms, as brown and dark-green pellets. Green pellets, composed of highly expandable, montmorillonite-type glauconite, are particularly common around the 100 fathom isobath. Both chamosite and glauconite have a high magnesium content, which seems to be usual during their early stages of formation.The formation of chamosite and glauconite is governed by redox potential and the availability of iron. If no reduction takes place, the pellets remain grey and their composition is similar to that of the clay matrix. Grey pellets are less restricted to a particular depth than are the chamosite and glauconite pellets, but distinct maxima occur around the 250 fathom isobath.

Distribution of detrital minerals in recent carbonate sediments from the Shaul Shelf, Northern Australia

Abstract Detrital minerals in Recent sediments from the Sahul Shelf show a well‐defined distribution pattern which can be related to nearby river estuaries. Two major contrasting heavy mineral provinces are evident, characterized in turn by an unstable and a stable suite of minerals. A zone of relatively high feldspar content coincides with the unstable heavy mineral province. The source of the detrital grains is considered to be the dissected lateritic hinterland, and the depth of dissection in any area may determine whether stable or unstable minerals are supplied to the ocean.