The Stream Sediment Geochemistry of the Walawe Ganga Basin of Sri Lanka - Implications for Gondwana Mineralization |
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| Authors: | Rohana Chandrajith CB Dissanayake HJ Tobschall |
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| Institution: | 1. Institute of Geology and Mineralogy, University of Erlangen-Nürnberg, Schlossgarten 5, D-91054 Erlangen, Germany;2. Department of Geology, University of Peradeniya, Peradeniya, Sri Lanka;1. Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur, West Bengal, 721 302, India;2. Radiochemistry Division, Variable Energy Cyclotron Centre, BARC, Kolkata, West Bengal, 700 064, India;1. Universidade Federal Fluminense, Av. dos Trabalhadores 420 – Vila Sta. Cecília, CEP 27255-125 Volta Redonda, RJ, Brazil;2. Centro de Tecnologia Mineral, Avenida Pedro Calmon, 900 – Cidade Universitária, CEP 21941-908 Rio de Janeiro, RJ, Brazil;3. Centro Federal de Tecnologia, Rua do Areal, 522, Pq Mambucaba, Angra dos Reis, CEP 23953-030 Rio de Janeiro, RJ, Brazil |
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| Abstract: | A regional geochemical and mineralogical study aimed at investigating the mineralization in the western-part of the Walawe Ganga (river) Basin in Sri Lanka is represented in this paper. The river basin is the 3rd largest in the country and has within it a boundary zone between two geologically different crustal blocks, which are marked by granulitic grade rocks and amphibolite grade rocks. Size fractions of stream sediments (< 63 μm; 63–125 μm; 125–177 μm and 177–250 μm) developed on the granulite-grade metamorphic terrain have been analysed at their source for their mineralogical and selected element compositions. Thirty-eight (38) sediment samples and 15 representative probable parent rock samples were chemically analysed giving special emphasis to the High Field Strength trace Elements (HFSE) including the Rare Earth Elements (REE). The granulite grade rocks in the study area is geochemically similar to that of post Archean upper crust. However the stream sediments developed from the high-grade rocks during the intense weathering, are markedly enriched with HFSE and REE. The enrichment of HFSE and LREE is accounted for by the presence of HFSE- and REE- rich accessory mineral phases such as zircon, monazite, apatite, garnet and rutile in the sediments. In some samples, the content of heavy minerals contributes as much as 50 wt. %. These minerals act as a source of elements in the sediments. However, extreme hydraulic sorting of HFSE- and REE-bearing minerals during the sediment deposition cannot be expected within a short distance from near the sources except from a mineralized occurrence. Therefore, the higher enrichment of these elements presumably indicates occurrences of scattered mineral sources such as highly differentiated granites and associated pegmatites within the Walawe Ganga drainage basin. These granitic pegmatites are probably intruded during or soon after the main granulite-facies metamorphic event and similar events are seen in other terrains of East-Gondwana. |
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| Keywords: | Stream sediment geochemistry Walawe Ganga Basin Sri Lanka |
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