Tur Ghar occupies the northeastern side of Kandahar city and some parts of ShawaliKot and Daman Districts. Such Cretaceous volcanogenic formation containing Hematite veins, fan alluvium foothills,...
WhatsApp: +86 18221755073of basalts and komatiites (-15 Myr)22; and the horizontal length-scale of the 2.7-Gyr crustal anatectic event (1,000 km)22• The apparently short time interval for komatiite eruption sug ...
WhatsApp: +86 18221755073A dome-shaped ancient Buddhist shrine, the Topdara stupa to the north of Kabul was described by 19 th century British explorer Charles Masson as "perhaps the most complete and beautiful monument of the kind in these countries." Since Masson's visit in 1833, the Topdara stupa saw few visitors and had fallen into neglect until recently, in 2016, when an Afghan …
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WhatsApp: +86 18221755073Eastern Afghanistan In the ranges of eastern Afghanistan, two distinct ophiolite belts can be separated [5,10]. Major overthrusts and tectonic structures in the two belts show a …
WhatsApp: +86 18221755073In this study, we conduct detailed mineralogy, petrology and isotopic geochemistry on the Meso-Cenozoic alkaline basalts from the Tuoyun Basin in the western CAOB, which are exposed …
WhatsApp: +86 18221755073Tur Ghar occupies the northeastern side of Kandahar city and some parts of ShawaliKot and Daman Districts. Such Cretaceous volcanogenic formation containing Hematite veins, fan …
WhatsApp: +86 18221755073Afghanistan comprises a collage of many lithotectonic domains sutured together as block terranes on the southern Eurasian Plate by collisional tectonics throughout the Proterozoic and Phanerozoic.
WhatsApp: +86 18221755073The basalts from the eastern belt have Ni and Cu contents similar to those from the central belt and have Cu/Ni ratios of 0.3–0.6 (Table 2). All basalts have Ir, Ru, Rh, Pt, and Pd contents that are mostly below 1 ppb (Table 2). The PGE contents in basalts from the western belt are slightly higher than those of basalts from the other two belts.
WhatsApp: +86 18221755073These basalts, together with Wulanhada and Siziwangqi basalts reported in this study, constitute a SW-NE profile. Basalts distributed in this profile have similarly high δ 66 Zn values, indicating that the amounts of recycled carbonate in their sources are similar. In other words, this profile is nearly vertical to the subducted direction of ...
WhatsApp: +86 18221755073in northern Afghanistan and the Pamirs is substantiated for the first time. In Iran, three blocks are traditionally defined: Elburz, Central Eastern Iran (Lut Massif included), and ... basalts belong to either N-MORB and E-MORB types or calc-alkaline (subduction-related) series [6]. Basalts with a K–Ar age of 88–77 Ma underlie Maastrichtian
WhatsApp: +86 18221755073The theory of plate tectonic has been accepted to explain the origin of mafic igneous rocks such as island arc basalts (IAB) at convergent plate boundaries and mid-oceanic ridge basalts (MORB) at divergent plate boundaries (e.g., Hofmann, 2014; Rooney et al., 2014; Stern, 2002; Zheng et al., 2020).Although ocean island basalts (OIB) and continental basalts also …
WhatsApp: +86 18221755073Basalt Properties . Color: While typically described as black, basalt can exhibit a range of hues due to variations in mineral composition and oxidation. Shades of grey, green, and even reddish-brown are possible. Texture: Basalt exhibits a wide range of textures, from fine-grained and aphanitic (almost glass-like) to coarse-grained and porphyritic (containing larger crystals within …
WhatsApp: +86 18221755073The basalts generally show a positive correlation between Zr and high field strength elements (HFSE, such as Ti and Nb), rare earth elements (REE) and Th, suggesting that these elements were immobile during alteration. In contrast, the lack of correlations between Zr and low field strength elements (LFSE: Cs, Rb, Ba) suggests the mobility of ...
WhatsApp: +86 18221755073A volcanic-sedimentary succession of Paleogene age is exposed in isolated patches at the southern margin of the Tajik block in the Ghor province of Central Afghanistan. The …
WhatsApp: +86 18221755073The fields of the island arc basalts and NEB are from Kepezhinskas et al. (1996). The field of the Luotuogou and Tuwu Carboniferous basalts is constructed using data from the following sources: Xia et al., 2004b; unpublished data of Q. Wang. Data sources for the igneous rocks in the Alataw area are the same as in Fig. 4.
WhatsApp: +86 18221755073The arc lithosphere is a key suspect for derivation of the low-titanium basalts because (1) the geochemical and isotopic signature of the low-titanium basalts has very similar characteristics to rocks formed in subduction settings [e.g., Kelemen et al., 2003]; (2) arc crust is exposed beneath the Nikolai basalts in Alaska; and (3) the low ...
WhatsApp: +86 18221755073Pb–Nd–Hf isotope characteristics indicate that the carbonated eclogite-derived melts likely originated from the stagnant Pacific slab. Although Cenozoic basalts from both the east of the NSGL (ENSGL) and DVF domains exhibit light δ 26 Mg values, basalts from the ENSGL nevertheless have lower δ 26 Mg values than those in the DVF domain ...
WhatsApp: +86 18221755073Saccani et al. (2022) have shown that metabasalts are represented by three geochemically distinct protoliths, including sub-alkaline basalts showing either N-MORB or E-MORB compositions and ...
WhatsApp: +86 18221755073basalts in afghanistan. basalt, extrusive igneous (volcanic) rock that is low in silica content, dark in colour, and comparatively rich in iron and magnesium. Some basalts are quite glassy (tachylytes), …
WhatsApp: +86 18221755073They are always altered, serpentinized, or epidotized. However, olivine basalts have been identified that differ from volcanic rocks (mainly andesites) in the Lower Cretaceous of the same region (see below, Triassic of the Kabul Block).
WhatsApp: +86 18221755073There are several major tectonic units in the Logar area: the basement of the Central Afghanistan Terrane, the platform-type cover sequence of the Kabul Terrane and the Logar Ophiolite Complex.
WhatsApp: +86 18221755073Miocene to Quaternary alkali basalts in the Lut–Sistan region, eastern Iran are spatially associated with two active, N–S-trending dextral strike–slip fault systems in the region, i.e., the Neh faults in the Sistan suture zone and the Nayband fault ~ 200 km further to the west in the Lut block.Here, we present new 40 Ar/ 39 Ar ages, geochemical and Sr–Nd isotopic data …
WhatsApp: +86 18221755073The study area, Maychew, is located in the northern eastern corner of the northwestern Ethiopian plateau. Petrological, petrographic, and geochemical (trace and major elements) data are presented and integrated for Maychew flood basalts to characterize the geochemistry and constrain petrogenetic processes involved in the evolution of these flood basalts.
WhatsApp: +86 18221755073The basalts unconformably overlie lowermost Permian diamictites, with locally intervening black shales and debris flow deposits, and are followed in turn by chert-bearing quartzarenites and silty to phosphatic marls yielding brachiopods of Roadian–Wordian age. ... Afghanistan, South Tibet, Myanmar, Thailand) began in the Early Carboniferous ...
WhatsApp: +86 18221755073Northern Afghanistan is part of the continental shelf of the southern Eurasian plate, including the Afghan-Tajik and Amu Darya basins (Fig. 3). Northern Afghanistan is relatively …
WhatsApp: +86 18221755073Mare basalts on the lunar surface are tangible expressions of the complex thermal evolution and geological processes that have occurred within the lunar interior. These basaltic manifestations are ...
WhatsApp: +86 18221755073The decoupling of high Sr contents and depleted Sr Nd isotopes in the alkali basalts indicate that the mantle carbonation is subjected to recent subduction events and is possibly related to the subduction of the Neo-Tethyan seafloor. The calculated melting temperature of these basalts are generally high (1487–1583 °C), which is consistent with that of Cenozoic …
WhatsApp: +86 18221755073Afghanistan and surrounding regions present a mosaic of continental blocks originating from Gondwanaland [42,44]. The Hercynian orogeny belt, characterized by …
WhatsApp: +86 18221755073The basalts in the fluid flow conduits interacted with medium- to high-temperature hydrothermal fluids and were silicified, leading to enrichment in Co, Cu, Zn, and U, and depletion in Mg, Fe, Ca, Mn, Li, Rb, Cs, and REEs. Fluids that flowed through the rubble mixed with large amounts of seawater, resulting in variable degrees of saponite ...
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