Conceptual Exploration for Tin, Gold and Diamond Placer Deposits in ‘Sundaland’ (Indonesia and Malaysia) by Understanding the Late Cainozoic Stratigraphic Context

The Australasian Institute of Mining and Metallurgy
D A-F Batchelor
Organization:
The Australasian Institute of Mining and Metallurgy
Pages:
8
File Size:
1780 KB
Publication Date:
Mar 18, 2015

Abstract

"An EXTENDED ABSTRACT is available for download. A full-length paper was not prepared for this presentation.South-East Asia represents the world’s most productive tin province, mainly from placers. Kalimantan has been a major diamond producer, while in the 1980s a placer gold rush occurred in Indonesia and Malaysia. Reviewing extensive geological and mining data highlights phenomenal palaeo-environmental changes in the Sundaland region, interpreted to be responsible for generating ‘giant’ placers. Correlation of the Late Cainozoic stratigraphy has been facilitated from mine exposures and drill holes distributed throughout Peninsular Malaysia, the Indonesian Tin islands and Kalimantan, including contiguous marine areas with extensive shallow seismic profiling data. Knowing the association of rich placers with palaeo-environmental episodes and stratigraphical units has been helpful to facilitate their discovery. All three placer commodities responded similarly to region-wide landscape evolution following Mio-Pliocene high sea levels. Commencing with major regression, important stages comprised: a long period of landscape stability with deep weathering during the maximum Sundaland extent gradually rising sea levels/precipitation initiated slumping of mineralised regolith to form fans, later reworked by braided streams with aggradation (Old Alluvium); during episodic pluvial periods downcutting upgraded placers significant change occurred around Middle Pleistocene time with peneplanation and pedogenesis from Late Pleistocene time ‘modern’ fluviatile deposition (Young Alluvium) filled incised V-shaped valleys.Placer seams show systematic variation in stratigraphic position, in particular cassiterite especially occurs in the Old Alluvium (equivalent Upper Dahor Formation in Kalimantan). Gold is commonly richer in gravelly younger deposits, partly because of secondary precipitation within permeable alluvium. Reworked diamonds are predominantly concentrated especially in younger fluviatile alluvium.CITATION:Batchelor, D A-F, 2015. Conceptual exploration for tin, gold and diamond placer deposits in ‘Sundaland’ (Indonesia and Malaysia) by understanding the late Cainozoic stratigraphic context, in Proceedings PACRIM 2015 Congress, pp 499–506 (The Australasian Institute of Mining and Metallurgy: Melbourne)."
Citation

APA: D A-F Batchelor  (2015)  Conceptual Exploration for Tin, Gold and Diamond Placer Deposits in ‘Sundaland’ (Indonesia and Malaysia) by Understanding the Late Cainozoic Stratigraphic Context

MLA: D A-F Batchelor Conceptual Exploration for Tin, Gold and Diamond Placer Deposits in ‘Sundaland’ (Indonesia and Malaysia) by Understanding the Late Cainozoic Stratigraphic Context. The Australasian Institute of Mining and Metallurgy, 2015.

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