Abstract:
The beach placers are largely composed of resistant heavy minerals and are known as one of the most
easily exploitable mineral deposits in the world. Such placers are commonly deposited along the edges
of large water bodies due to the gravity separation processes. The southeastern coast of Sri Lanka
contains extensive depositional beaches, lagoons, and estuaries, and shows signs of occurrences of
valuable mineral placers. We investigated the mineralogy and micro textural features of placer and
non-placer sediments in the lagoonal beaches (Periya Kalapuwa, Korai, Komari, Pottuvil and Arugam
Kalapuwa) and Heda Oya riverine beach of the southeastern part of Sri Lanka. The study aimed to
compare transport and depositional processes, and paleoenvironmental histories of placer and nonplacer deposits. The field and mineralogical results revealed that the sediments in the lagoonal shores
are black-colored ilmenite placers with abundant ilmenite and accessory zircon while the sediments
from Heda Oya riverine shore are red-colored titanium placers with almandine. The non-placer
deposits are mostly composed of quartz, albite, and magnesian calcite. The micro-textural analyses of
240 quartz grains from placer and non-placer deposits showed the presence of twenty-five predefined
micro-textures indicating the prevailed influences of subaqueous-beach, fluvial, aeolian, and chemical
alteration processes on the sediments. Also, these textures showed a decrease in source-sinking
distances and subaqueous beach processes, while an increase in fluvial processes from non-placer, red
placer to black placer deposits. Chemical alteration processes such as cracks and solution pits are
higher in heavy placer deposits revealing the deposition in the steady low energy environment.
Further, the cross-cutting relationships between environment specific micro-textures show crystalline
overgrowth cross-cutting on chemically modified surfaces, upturned plates with cracks and solution
pits, and large conchoidal fractures cross-cutting on surfaces that contain V-shaped percussion cracks.
The cross-cutting relations indicate prevailed pre-aeolian processes and post-chemical alteration
processes on placer deposits. Further, they are more recently controlled by subaqueous beach
processes with sparse aeolian contributions. Large conchoidal fractures, arcuate and straight steps
micro-textures, and mineralogical contents of the placer deposits indicated crystalline rock sources.
Hence, these placer deposits probably have been derived from granitic gneiss, granodioritic gneiss,
charnockites and garnet-bearing granulites of the Precambrian Vijayan Complex and Highland-Vijayan
tectonic boundary zone.
