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There is evidence many were used as prostitutes by the soldiers.
Centuries ago, the British East India Company used a private navy against piracy in the same waters with much success.
Heavy mineral correlation belongs to the third of these categories.
It is one of a family of provenance-based tools that also includes chemostratigraphy [4,5], Sm-Nd isotope stratigraphy [6,7] and clay mineral stratigraphy [8,9].
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Geology is typically broken up into two major fields of study: physical geology, historical Geology.
Physical Geology examines the materials composing Earth and seeks to understand the processes that operate beneath the surface; think of it as the how and why of Geology.
The examples cover Triassic red-bed successions in the central North Sea and west of Shetland, which have been subdivided and correlated using provenance-sensitive ratio data and mineral morphologies; Middle Jurassic paralic sandstones in the northern North Sea, correlated using garnet geochemistry; Upper Jurassic deep water sandstones in the northern North Sea, discriminated using rutile geochemistry and detrital zircon age data; and the “real-time” application of the technique at well site in Devonian-Carboniferous fluvio-lacustrine sandstones of the Clair Field, west of Shetland.
One of the most important practical economic applications of heavy mineral analysis is the correlation of sandstones that host reserves of oil and gas.