卜闻
发表于 2025-3-28 14:37:51
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Inveterate
发表于 2025-3-28 20:05:52
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Flat-Feet
发表于 2025-3-29 01:08:43
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过度
发表于 2025-3-29 04:05:30
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吞噬
发表于 2025-3-29 09:25:30
A Composite Structure of the Bashkir Anticlinorium: Insights from Detrital Zircons Search in Ordovicgrated characteristics of the studied dZr provide new constraints for their primary sources. A comparison of obtained data with rock types, U-Pb and Hf model ages of the crystalline complexes of the of Volga-Uralia basement, as well as characteristics of dZr from Late Precambrian strata of the Bashk
limber
发表于 2025-3-29 14:58:22
Structure and Geological Processes of the Earth: Seismic Evidences from the Indian Shieldtion of plate tectonics since Neoarchean. Further, they suggest differences in mode of subduction process during these periods. They provide evidences for the associated processes, like delamination, asthenospheric upwelling, and generation of younger Moho due to crust-mantle interaction. Evolution
高深莫测
发表于 2025-3-29 16:35:25
World Class Hutti Gold Deposit—An Archean Orogenic Gold Deposit in Hutti-Maski Greenstone Belt, Karn in relative- and absolute-timings. This contribution explores the variability in deposit characteristics, and its implications for generic genetic models for this deposit-class. Gold mineralization is confined to sub-parallel reefs hosted within sheared metabasalts. Mining is in progress in six out
Tincture
发表于 2025-3-29 20:55:28
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Anthrp
发表于 2025-3-30 02:02:53
Petrology and Geochemistry of Mafic–Ultramafic Rocks from Taka Area, Western Bastar Craton, Central rmalized REE patterns, namely a flat pattern with low HREE and fractionated LREE depleted pattern are observed. The IPGE (Ir, Ru) enrichment relative to PPGE (Pd, Pt, Rh) and the relatively low Pd/Ir values suggest that their parental melts were produced by melting of a moderately depleted peridotit
密切关系
发表于 2025-3-30 07:16:18
Tectonic Evolution of Babina–Prithvipur Crustal Shear Zones, Bundelkhand Craton, India: Implicationsipur shear zone (syn-to post-tectonic D. phase). These sheared rocks are characterized by the E-W to ESE-WNW trending mylonitic foliation and stretching lineation. The mylonitic foliation, asymmetrical rotated porhyroclasts (σa and σb mantled clasts), asymmetrical pressure shadows and deformation la