The 2018–2019 excavation of the Xiwubi site in Jiangxian County, Shanxi

2021 ◽  
Vol 21 (1) ◽  
pp. 47-74

Abstract A series of excavations were conducted at the Xiwubi site during 2018–2019, yielding abundant copper metallurgy remains dating to the Erlitou and Erligang cultural periods. Archaeological features include remains of smelting furnaces, charcoal kilns, houses, and refuse pits. A variety of artifacts were retrieved, ranging from copper ores, fragments of smelting furnaces, crucibles, and slag to objects made of pottery, stone, and bone. It is the first copper metallurgy site found in the Zhongtiao Mountains in the vicinity of the heartland of the Xia and Shang dynasties. Characterized by early dates, large scale, and advanced specialization in copper metallurgy, the excavation of the Xiwubi site provides substantial materials for the study of mining and use of copper ore resources by the Xia and Shang dynasties, as well as interactions between copper metallurgy and the destiny of the royal courts.

Starinar ◽  
2016 ◽  
pp. 173-191
Author(s):  
Aleksandar Kapuran ◽  
Dragana Zivkovic ◽  
Nada Strbac

The last three years of archaeological investigations at the site Ru`ana in Banjsko Polje, in the immediate vicinity of Bor, have provided new evidence regarding the role of non-ferrous metallurgy in the economy of the prehistoric communities of north-eastern Serbia. The remains of metallurgical furnaces and a large amount of metallic slags at two neighbouring sites in the mentioned settlement reveal that locations with many installations for the thermal processing of copper ore existed in the Bronze Age. We believe, judging by the finds of material culture, that metallurgical activities in this area also continued into the Iron Age and, possibly, into the 4th century AD.


Author(s):  
William O'Brien

The Iberian Peninsula is one the most mineralized parts of Europe, with a long history of metal mining from prehistoric and Roman to modern times. The earliest evidence for copper metallurgy dates to the fifth millennium BC; however, distinctive Chalcolithic metalworking traditions did not emerge in most regions until 3000 BC onwards. There are widespread occurrences of copper mineralization in Spain and Portugal, including many areas with deposits of lead, tin, silver, and gold. Copper deposits occur in the Galician and Cantabrian mountain ranges of northern Spain, extending east to the Pyrenees. They are also numerous in central Spain, in the provinces of Madrid, Avila, Salamanca, and Segovia in the Central Range, and also in the Toledo and Betic mountains of Cordoba. Farther south, there are major copper deposits in the so-called Pyrite Belt, extending from Seville to Huelva into southern Portugal, and also in the Penibetic range from Cartagena to Malaga crossing the sierras of Almeria (Rovira 2002: fig. 3c; see Delibes de Castro and Montero Ruiz 1999 for regional surveys of copper deposits and indications of early mining; also Gómez Ramos 1999; Hunt Ortiz 2003). The widespread availability of ore deposits was a significant factor in the establishment of copper metallurgy in Iberia. How early is contentious, as is the means by which the new technology first developed in different parts of the peninsula. The older explanation of metal-seeking colonists from the east Mediterranean introducing this technology to southern Spain was replaced in the 1960s by a model that emphasized autonomous development (Renfrew 1967, 1973; Montero Ruiz 1994). This was based on the apparent antiquity of copper mining and metallurgy in Iberia and the distinctive technological processes that developed there relative to other parts of Europe. The earliest indication of copper metallurgy in Iberia may come from the settlement of Cerro Virtud in Almeria, south-west Spain. A single sherd from a metallurgical crucible used to reduce oxidized copper ore was discovered in a layer dated to the early fifth millennium BC (Montero Ruiz and Ruíz Taboada 1996; Ruíz Taboada and Montero Ruiz 1999).


1992 ◽  
Vol 24 (3) ◽  
pp. 507-550 ◽  
Author(s):  
Luis Valenzuela

This article looks at the beginnings and early development of the modern copper smelting industry in Chile. It analyses the factors which led to its occurrence, contrasting it with other countries where no smelting industry developed. It argues that the development of the Chilean smelting industry stimulated copper mining and reinforced the expansion of coal mining. Furthermore, it permitted the retention in the country of a larger part of the rent generated by copper mining than would have been the case had all the copper ore been exported, and was therefore an important factor in the development of the Chilean economy as a whole.Until 1879 tne Chilean copper industry was the most dynamic sector of the economy of the Republic. During the period 1844—79 it generated exports of 341 million pesos (around £64 million), or 42.3 % of the total value of the exports of the country, and contributed 29 million pesos, or almost 10% of the ordinary fiscal income, through the export duty levied.1 Most of this copper left Chile in the shape of ingots of over 99% fine (that is pure) copper, bar copper of c. 96 % fine or regulus, a semi-processed form of copper of around 50% fine; only 12.1 % left in the shape of copper ores of different types.2 The smelting and, to an even greater extent, the refining of the copper ore in Chile permitted the miners to develop a wider variety of potential markets. It also facilitated the Luis Valenzuela is a Lecturer at the Centre for Development Studies, University College of Swansea.


1982 ◽  
Vol 48 (1) ◽  
pp. 459-465 ◽  
Author(s):  
R. F. Tylecote ◽  
P. T. Craddock

Jovanovič has recently drawn attention to the early copper mine at Rudna Glava in the copper mining area of Maidanpek-Bor in Eastern Serbia (Jovanovič 1979, 103). This copper deposit has iron associated with it. In some respects this occurrence of iron and copper together compares with the deposit at Phalabora in South Africa where copper and other minerals are mined today. Rudna Glava has been a copper mine in the Chalcolithic period and an iron mine in the Turkish period. Today it is worked out, but the working of the iron ore has left exposed some of the shafts and galleries used by Chalcolithic and Bronze Age copper miners. It has been possible to obtain a sample of the copper ores used in the early periods and integrate them into a smelting programme (Tylecote et al. 1977, 305), the main purpose of which has been to determine the partitioning of the three elements between the ore, the slag and the metal. The object of this exercise was to try and relate the artefacts, the slag, and metal to the ore source. So far, ores from the British Isles, Spain, and Africa have been examined and reported (Tylecote 1977). The sample from Yugoslavia came rather too late for the first report but the work is continuing.The smelting work described in this report was carried out by Ali Ghaznavi and the analyses were kindly made by R. Hetherington formerly of Newcastle University and Dr P. T. Craddock of the British Museum Research Laboratory. I have to thank Dr B. Jovanovič of the Archaeological Institute, Belgrade, for supplying the material and inspiring the work.


Author(s):  
N. Zhalgasuly ◽  
A. V. Kogut ◽  
A. A. Ismailova

In the conditions of the Zhezkazgan copper deposit, which is worked underground, the losses of ore in the left pillars fluctuate from 12 to  25 %, sometimes reaching 40%. During the development of the  Zhezkazgan deposit, tens of millions of tons of rich ore were left in  various kinds of losses. The annual increase in ore losses in various  parts, taking into account the increasing production, is  approximately equal to the annual productivity of the whole mine.  Also in the production process so far rich in content of the interlayer  copper ores of low power. Therefore, the search for the most  effective methods of mining lost, off-balance and waste ores is of  paramount importance. One of such methods is underground  leaching, which allows to carry out their secondary development and make maximum use of the mineral wealth. The aim of the research  was to experimentally study the leaching of oxidized, mixed and  sulphide copper ores of the old spent mines in the Zhezkazgan deposit using various solvents. The squeezing of oxide  and sulphide rudes was carried out in 2 stages, when the durability  of the experimental crests was 35 hours and the durable 294 hours.  The oxidant-sulphide ore is 20 mm high and can be cured at 50-80  % media, for 10 months. For the period of time, the chalcocin rudus  is derived from 30 to 50 % of media, and from 5 to 12 % of bernital  chalcopyrite, which results in the effectiveness of the subsequent  method of squeezing the effluent. The best dissolves are acidic acid  (5-10 g/l) and acidified sulphate oxide (5 g/l). Residual cystic acid  production and development of oxidant processes up to 1.6-3.2 t/t  for medium oxidized rudder and up to 2.54.1 t/t for chalcocin rudder, which acts as a catalyst for thawing technical and economic indicators.


2021 ◽  
Vol 3 (4) ◽  
Author(s):  
S. Kekelia ◽  
Nona Gagnidze ◽  
I. Mshvenieradze ◽  
G. Kharazishvili

The paper presents brief characteristics of geological environments of ore deposit occurrences in Turkey, Georgia and Armenia. They can be attributed to Kuroko-type deposits, being distinguished by the character of ore accumulation. To the west, in Turkey, there are epigenetic and hydrothermal-sedimentary copper-zinc deposits that were formed in deep restricted basinal settings. An example of the latter is the Chayeli deposit.To the east, in the Caucasus, we have predominantly only epigenetic deposits. Besides, in the Bolnisi mining district (Georgia) there is the Madneuli deposit which represents an example of polyformational deposit. Here, within the restricted territory, have been concentrated:barite, barite-polymetallic, gold-bearing secondary quartzite, large-scale stockworks of copper ores. Judged by the 87Sr/86Sr ratios, some volcanites which are spatially associated with ores, might have been products of the “differentiation” of undepleted mantle, or other magmas that were generated in the lower part of the earth crust.In the Alaverdi ore district in Armenia, there are Jurassic volcanodepressions that host copper, copper-zinc and barite-sulfide ores. All the deposits of the Alaverdi district, porphyry copper including, contain economic reserves of ores.On the basis of available literature material and our own data, there has been created a mental-logical geological-genetic model of volcanogenic deposits.


2009 ◽  
Vol 71-73 ◽  
pp. 405-408
Author(s):  
Jochen Petersen ◽  
Sanet H. Minnaar ◽  
Chris A. du Plessis

During large-scale column tests at BHP Billiton’s Johannesburg Technology Centre (JTC) during 2005/6 on a low-grade copper ore, the concentrations of both oxygen and CO2 were continuously monitored in feed and exit gas as well as at various intermediate positions over the height of the column. This paper describes results from a test run at 40 °C fed with an air stream enriched to between 1000 and 2000 ppm CO2. Oxygen consumption very closely tracks iron and copper leaching. CO2 is consumed rapidly from the bottom up, resulting in significant depletion midway through the column, even though an enriched feed was used. Oxidation rates decline in CO2 depleted zones, but were not observed to cease completely. This rate of decline is postulated to be linked to a slowly decaying population unable to regenerate itself. Comparison between O2 and CO2 consumption rates shows a linear correlation beyond a minimum oxidation rate. This minimum rate corresponds to a non-growth maintenance energy requirement, and the slope of the linear correlation to the growth yield. Both are functions of available CO2 in the range 50 to 1000 ppm, with maintenance declining and yield increasing. The findings of this study imply that CO2 supplementation in bioheaps will stimulate microbial growth and CO2 consumption, but not necessarily increase the rate of oxygen uptake and hence leaching. Absence of CO2 is expected to result in gradual population decline, but a degree of oxidation continues on the basis of maintenance. In tall heaps CO2 depletion with height is likely and may therefore result in impaired leaching in the upper zones.


1994 ◽  
Vol 60 (1) ◽  
pp. 245-286 ◽  
Author(s):  
Andrew Dutton ◽  
Peter J. Fasham ◽  
D. A. Jenkins ◽  
A. E. Caseldine ◽  
S. Hamilton-Dyer

The discovery of evidence to suggest that copper ore was exploited at the Great Orme on a considerable scale in prehistory is of great significance in our understanding of the development of metalworking technology in the British Isles.In the past, the apparent absence from the archaeological record of a contemporaneous native mineral source for the production of copper and copper alloy artefacts during the Bronze Age has led to the assumption that raw materials, as well as metal technology, were imported from abroad. Alternatively, whilst accepting that local resources could have been exploited, it was assumed that these would have been obliterated by the mining operations of later centuries.There are now several sites on the British mainland and in Ireland which have been identified and dated as having been exploited for copper ores during the Bronze Age, of which a number, as on the Great Orme, had since seen intensive working during the 18th and 19th centuries AD. AS yet, much of the evidence has come essentially from surface excavations, but at the Great Orme surface excavation combined with underground exploration has revealed a system of workings of truly remarkable size. A series of 10 radiocarbon dates has been obtained from within the mine complex, indicating that working was carried out for over a thousand years spanning the Early to Late Bronze Age.The true extent of the surviving prehistoric workings is yet to be realized but present evidence indicates mining activity covering an area in excess of 24,000 square metres, incorporating passages totalling upwards of 5 km, penetrating to a vertical depth of 70 m.Much of the archaeological evidence contained within this report has been gained from detailed excavation carried out within surface workings, which in their own right constitute a sizeable part of the prehistoric mine. From the surface area presently exposed it is conservatively estimated that 40,000 cubic metres of material was removed during the Bronze Age. Much of the early technology represented within the surface workings reflects the technology employed in the deep workings, with the additional evidence of ancillary operations which would seem to relate solely to surface locations.Whilst the excavations reported in this paper relate to surface, or near surface, workings, they must be seen in the context of a labyrinthine complex of prehistoric workings recorded at depths of over yom (Jenkins & Lewis 1991; Lewis 1994). These deep workings are the subject of parallel studies to be reported elsewhere. The known underground and surface prehistoric workings are on a scale so far unparallelled in Britain and are of international significance. Elsewhere in Europe there is evidence for the mining of copper ores at Ai Bunar in Bulgaria dated to 5840 BC (Cernych 1978) and at Rudna Glava in former Yugoslavia dated to 4715 BC (Jovanovic 1979). Evidence for subsequent copper mining has been dated to 3785 BC in southern Spain (Rio Tinto area: Rothenburg & Blanco Freijeiro 1980) and to 3330 BC in Austria (Mitterberg; Pittioni 1951), marking an apparent development and extension westwards and northwards of copper technology. More recently, the dating of two sites in the south of France to around 3330 BC, at Cabrieres (Ambert et al. 1990) and Bouche Payrol, near Brusque (Barge 1985), has confirmed another area of Bronze Age working.


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