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Not all metal deposits have igneous origins- sedimentary deposits can also be a valuable source of many metals, including copper. While sedimentary copper deposits share the feature of a sedimentary origin- there are many different types of sedimentary copper deposits- each with distinct characteristics.
By Leia Michele Toovey- Exclusive to Copper Investing News
Sedimentary deposits are generally stratiform- meaning their morphology is controlled by stratigraphy of their host rocks. Sedimentary deposits are generally tabular, sheet-like or flat lenticular form. They are horizontal if not disturbed, but are frequently folded and faulted. Beds containing metallic ore are generally less than 20 ft. thick. Beyond copper, common metals found in sedimentary deposits are lead, zinc, cobalt and silver.
Sedimentary copper can be deposited through different processes. However, the formation is the result of the movement of a copper-bearing fluid through strata, that for one reason or another precipitates. Precipitation is generally due to a of chemical change, either through the contact of certain host rocks, or as in the case with sedimentary exhalative deposits, through contact with water. Sedimentary copper may be deposited in the pore spaces of permeable rocks, or in faults and fractures. A common cause of precipitation is when copper-bearing fluids across a reduction front, resulting in the precipitation of copper sulfides. While sedimentary rock-hosted stratiform deposits are relatively common- large sized deposits are not. Currently, supergiant deposits arerecognized in only three basins: the Paleoproterozoic Kodaro-Udokanbasin of Siberia, the Neoproterozoic Katangan basin of south-central Africa, and the Permian Zechstein basin of northern Europe.
Copper-bearing sandstones and shales
Copper can be deposited in sandstones and shales from the precipitation of metals from fluids circulating in the host rock. Geologists’ have differing opinions as to whether this generally happens at the time the host rocks were deposited or later on, but both schools of thought agree that the minerals were deposited when the fluids reached a “chemical trap”, a place where the chemistry of the rock changed in a way that made it impossible for the metals to remain in solution. Examples of copper-bearing sandstones can be found in Zambia and the Democratic Republic of Congo.
Red-bed deposits
Red-bed deposits are named, obviously so, due to their red coloration, which is the result of oxidation of the rocks after exposure to the atmosphere. There are two distinct types of red-bed deposits, volcanic and sedimentary. The volcanic variety is of more economic importance than the sedimentary; however, in this article we will keep our focus on the sedimentary variety. Sedimentary red-bed deposits are relatively small, and as a result are rarely mined. Currently, two known producers are the Dzhezkazgan deposits of central Kazakstan and the Paoli deposit of Oklahoma.
Kupferschiefer-type deposits
These large, regionally extensive deposits are similar to the red-bed type. Kupferschiefer-type deposits form in a transitory marine-terrestrial environment, most likely created by the gradual submergence of land by a shallow sea. Kupferschiefer deposits are a result of red-beds, formed in a terrestrial setting, being overlain by reduced marine sedimentary rocks.
Sedimentary Exhalative Deposits
SedEx deposits are formed when hydrothermal fluids enter a water reservoir, such as an ocean, and precipitate minerals. SedEx deposits are the world’s most important lead and zinc source, and a secondary source of copper.
Sedimentary copper miners and explorers
TNG recently acquired the McArthur River tenement, 50 kilometers south of the township of McArthur in Australia. A maiden exploration program is currently underway on the property. The tenement includes numerous prospective copper targets identified from previous stream sampling results and prospective geology. Exploration will be aimed at large scale sedimentary hosted copper deposits similar to Mount Isa and Gunpowder in Queensland and the large copper deposits of Zambia and the Democratic Republic of Congo.
Caribou Copper Resources Ltd. (TSXV:CKR)
Owns the Caribou Dome property, located in the Talkeetna mining district of Alaska. The Caribou Dome Prospect is located on the transition zone between a belt of volcanic rocks and a sequence of sedimentary rocks, and the primary resource target is copper.
Playfair Mining Ltd. (TSXV:PLY)
Owns 100% interest in the copper-silver Seal Lake project located in central Labrador, Canada. The property covers a sediment hosted stratiform copper-silver system that hosts 136 copper-silver occurrences. The stratigraphy and host rocks at Seal Lake are similar to the rocks hosting the world-famous White Pine copper-silver district in Michigan.