The Relationship of Mineral Deposits to Early Crustal Evolution
The Archean accounts for approximately half the recorded history of the earth, comprising over 2,000 m.y. of geologic time. As the first ~800 m.y. are virtually lost from the record, events on the surface of the planet can only be speculated over. It is probable that this formative episode was magmatically turbulent and culminated with the final stages of meteorite bombardment ~3,900 m.y. ago. The next events, for which there is geologic evidence, involved the regions now represented by the high-grade gneiss terranes in which the first mineralization was developed. Ore deposits are not well represented in these regions for one or a combination of the following reasons: (1) mineral concentrations may have been recycled or destroyed during the initial turbulent episode of protocontinental development; (2) mineralization may have been destroyed by later tectono-thermal events that characterize the high-grade mobile belt regimes; or (3) mineralizing events or conditions may not have evolved sufficiently for metal concentrations to have formed in significant amounts.
The period of the Archean, beginning ~3,500 m.y. ago and terminating ~2,500 m.y. ago, witnessed the development of the low-grade granite-greenstone terranes of the shield areas. An examination of the principal components of these regions is undertaken following an existing model whereby greenstone sequences are subdivided into a basal unit comprising mainly mafic-ultramafic rock types, followed by an upper mafic to felsic volcanogenic succession, the latter succeeded by an essentially sedimentary group of rocks.
The nature and distribution of Archean mineralization associated with the granite-greenstone terranes is described, and it is shown that there is a strong genetic link between mineral types and rock compositions. Evolutionary trends in the nature and geochemistry of magma types are discussed, and these are considered to reflect changing conditions of heat flow, changes in the nature of the atmosphere and hydrosphere, and progressive modification of the earth’s crust resulting from protocontinental nucleation and development. Magma types ranging from komatiitic basalts and peridotites to calc-alkaline series basalts-dacites-rhyodacites-rhyolites suggest that geotectonic conditions have changed not only within individual greenstone belts but also over the time span of the entire Archean. Available information suggests that the island-arc or trench-back arc-marginal basin system provides the closest modern analogue to the ancient greenstone sequences. However, sufficient differences exist to caution against direct correlation with plate tectonic mechanisms operating at present, and it is suggested that the early Archean greenstone sequences may have been involved more with vertical tectonics in response to gravitational differences resulting from sinking volcanic piles and diapirically rising granitoid complexes. In later Archean times conditions might have approached those currently favored for Phanerozoic orogenesis.
Finally, it is suggested that Archean ore deposits are essentially secondary in origin, having formed mainly as a result of superimposed processes of igneous intrusion, metamorphism, structural disturbance, and chemical alteration acting on suitable host rocks during or after their formation and deposition.
Figures & Tables
Seventy-Fifth Anniversary Volume
The first notions of a new journal came to J. E. Spurr during the closing days of 1904. When he shared his thoughts with friends in Washington, D. C., they were so enthusiastic about the suggestion that they formed themselves into an ad-hoc committee to seek ways to implement the idea. The ad-hoc group met informally for several months and by May of the following year was ready to announce the birth of an unusual new publishing company and the journal the company would produce. The first formal meeting of the Economic Geology Publishing Company took place on May 16, 1905. The first issue of the new journal appeared in October of the same year, and the first volume was completed in December 1906. The birthing was not easy, but it was successful because the founders provided much of the financing as well as the first papers. The story of those earliest days and the many struggles of the fledgling journal is engagingly recounted by Alan M. Bateman in an article published in the Fiftieth Anniversary volume.
From inception, management of the journal has differed from the management of most scientific journals. There was no sponsoring society, so the founders raised capital by incorporating and selling shares in the venture. The journal has been owned and published by the Economic Geology Publishing Company ever since. There is no record that the founders experienced difficulties in selling shares in the Company, but they must have had some because the Publishing Company had a goal that other corporations(and presumably many of the investors) would have found difficulty in understanding: the new corporation was committed to keeping the books balanced but not to making a profit.
Initially incorporated in the District of Columbia, the Publishing Company was reincorporated in 1970 as a nonprofit membership corporation in Delaware. The modification in corporate status came in response to a suggestion made by the Internal Revenue Service.
The affairs of the Publishing Company are controlled by a Board of Directors, and the journal is sold to the public by direct subscription. Day-to-day operations of paper selection, review, and printing are in the hands of the Editor, while business matters, such as subscriptions and advertising, are in the hands of the Business Editor.
The one tie the Publishing Company has with a society was instituted many years after the journal. was founded—with the Society of Economic Geologists. When the Society was founded in 1920 it first considered publishing its own bulletin. Because the venture seemed financially questionable, and the coffers of the new society were bare, an arrangement was reached whereby members of the Society first received offPrints of papers written by its members and eventually Economic Geology as