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We show that if these problems are not adequately taken into account and tackled the result will be that fundamentally wrong life spans of porphyry systems will be estimated.We also provide basic guidelines to follow when trying to resolve the duration of magmatic-hydrothermal events in porphyry systems with the highest accuracy and precision currently achievable.The general and his wife are also each shown twice on the lid frieze, together holding each other's hands at the centre, and singly at the ends, again with unfinished faces.Pairs of figures of an older man and a woman stand beneath trophies at either end of the main face, uninvolved in the battle.
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This is so because the duration of magmatic-hydrothermal events in porphyry systems is instrumental to the development of genetic models necessary to explore a category of mineral deposits that provide most of the copper and significant amounts of base and precious metals to our economy.
The problem of determining the absolute duration of magmatic-hydrothermal events in porphyry systems has been addressed through thermal modeling of cooling intrusions and time needed to precipitate specified metal amounts from active hydrothermal systems with known metal concentrations and fluid fluxes.
These are at the same scale as the general, and all other the battling figures are smaller; indeed, in defiance of any attempt at perspective, the soldiers and horses at the "front" of the scene in the lower part are somewhat smaller than their equivalents at the "back" in the upper part.
Determining the absolute duration of magmatic-hydrothermal events leading to the formation of porphyry systems (i.e., including porphyry copper, skarn, and epithermal deposits) is one of the key questions in ore geology.
The Portonaccio sarcophagus is the best known and most elaborate of the main Antonine group, and shows both considerable similarities to the Great Ludovisi sarcophagus, the late outlier from about 250, and a considerable contrast in style and mood.