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This research deals with the study of geochemical, petrographic and mineralogical properties of Wolay Nephrite Occurrences in Kunar Province. Nephrite is a relatively silicate mineral, Cyclosilicate, with a chemical composition of Ca2(Mg,Fe)5Si8O22(OH)2 and has a monocline crystal shape. It is found in metamorphic rocks in many parts of the world. Wolay nephrite area is related to the tectonic zone of Jalalabad. Jalalabad zone is located in the eastern part of Afghanistan and south-east of the Nuristan zone. Correspondingly, this zone is related to the upper Cambrian or younger Cambrian. In this area, the age of rocks is related to Archean- Middle Proterozoic AR-PR2. This contribution presents the first systematic mineralogical and geochemical studies on the Wolay nephrite deposit. Electron probe microanalysis, X-ray fluorescence (XRF) spectrometry, inductively coupled plasma mass spectrometry (ICP-MS), and isotope ratio mass spectrometry was used to measure the mineralogy, bulk-rock chemistry, and stable (O and H) isotopes characteristics of samples from Kunar. Field investigation shows that the Kunar nephrite ore body occurs in the dolomitic marble near the intruding granitoids. Petrographic studies indicate that the nephrite is mainly composed of fine-grained actinolite with Schist and dolomite. Geochemical studies show that all nephrite samples have low bulk-rock Fe/(FeO + MgO) values (4.72–21.34%), as well as SiO2 (72.75%), Al2O3 (2.01), CaO (14.58%) and NiO (0.05%) contents. The chemical data analysis and interpretation of F=Mg/Mg+Fe percentages show that the Nephrites type is actinolite. The deposit of nephrite mineral has been formed in hydrothermally veins and lens shape in contact with serpentinite and carbonate (dolomite marble) rock in the under study area. The color and its clarity have a direct effect on the economy and its price. The Nephrite from the Khas Konur district is found in green color due to the existence of iron elements. [ABSTRACT FROM AUTHOR]

Subduction megathrusts below the land Moho slip at either steady creep or episodic slow slip events (SSEs). However, deformation styles and mechanisms responsible for aseismic megathrust slip remain unknown. We examined the subduction mélange in Kyushu, Japan, which consists of ultramafic, mafic, and sedimentary rocks. The mélange deformed at ∼470 °C under epidote-amphibolite facies condition, comparable to the inferred conditions of SSEs near the mantle wedge corner in the Nankai subduction zone. Subduction-related viscous shear in the mélange was concentrated into antigorite serpentinite and ultramafic schist mainly composed of chlorite and fine-grained actinolite, which is characterized by anastomosing scaly foliations and S C fabric. The mixing of mafic and ultramafic rocks in the mélange induced metasomatic reactions, resulting in the release of water from metasomatized mafic rock and the production of fine-grained actinolite in ultramafic schist. The fine-grained metasomatic actinolite exhibits chemical zoning of aluminum and truncation of the zoning parallel to S surface through dissolution-precipitation creep. Water released by metasomatic reactions may assist the dissolution-precipitation creep. Rheological analysis indicates that the dissolution-precipitation creep of fine-grained actinolite in ultramafic schist accommodated plate convergence and SSEs at shear stresses of 0.3–5 MPa and 10–40 MPa, respectively, whereas antigorite serpentinite can accommodate slow slip rates at shear stresses of ≤43–94 MPa, much higher than inferred shear stresses during SSEs in active subduction zones. The down-dip limit of the metasomatic reactions, determined from the stable condition of metasomatic actinolite in the ultramafic schist, was ∼40–50 km depth, comparable to the lower limit of the SSEs region in the Nankai subduction zone. We suggest that while antigorite serpentinite only accommodated aseismic creep, dissolution-precipitation creep of metasomatic actinolite in weaker ultramafic schist can host more diverse slip behavior including aseismic creep and SSEs. The metasomatic reaction between mafic and ultramafic rocks at the slab-mantle interface is potentially one of the factors controlling the downdip limit of SSEs below the land Moho. • Mélange deformation was concentrated into serpentinite and ultramafic schist. • Metasomatic reactions produce fine-grained actinolite in ultramafic schist. • Metasomatic reactions weaken ultramafic schist by promoting pressure solution creep. • Pressure solution creep of metasomatic actinolite can facilitate megathrust slip. • Metasomatic reaction may control downdip limit of slow slip event. [ABSTRACT FROM AUTHOR]