1996
DOI: 10.1126/science.273.5283.1819
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Copper Sources, Metal Production, and Metals Trade in Late Postclassic Mesoamerica

Abstract: Copper Sources, Metaldepends on whether regional geologic formation processes have resulted in clearly delineated LI fields, as well as on the num-Prod uction, and Meta 1s Trade i n ber of deposits analyzed. We considered a deposit or mining region to qualify as a Late Postcl assi Mesoa me i ca potential source when the artifact signature fell within the ore field. T o determine

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Cited by 52 publications
(70 citation statements)
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“…he results of research conducted in the late 1980's and early 1990's by Dorothy Hosler (1994;Hosler and MacFarlane, 1996) and more recently (Shugar, 2005(Shugar, , 2008 have provided valuable insights into the nature of Maya metallurgy during Postclassic and Spanish colonial times. he presence of several previously unknown copper artifact types at the site along with the results of recent chemical compositional and microstructural analysis greatly strengthen the argument for localized re-melting and casting of copper-base artifacts in the Maya Lowlands.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…he results of research conducted in the late 1980's and early 1990's by Dorothy Hosler (1994;Hosler and MacFarlane, 1996) and more recently (Shugar, 2005(Shugar, , 2008 have provided valuable insights into the nature of Maya metallurgy during Postclassic and Spanish colonial times. he presence of several previously unknown copper artifact types at the site along with the results of recent chemical compositional and microstructural analysis greatly strengthen the argument for localized re-melting and casting of copper-base artifacts in the Maya Lowlands.…”
Section: Discussionmentioning
confidence: 99%
“…Over 42% of the entire assemblage of copper-base artifacts from Lamanai consists of bells, most of which are plain walled and either pyriform or globular in shape (Figure 3). A total of 23 of the 79 (29%) total bells recovered thus far from Lamanai have been analysed to date (Hosler, 1994;Hosler and MacFarlane, 1996;Shugar, 2005Shugar, , 2008Williams, 1990 he results of LOM analyses revealed that all bells exhibited a similar large-grained microstructure that is typical of slow cooling of molten metal. his strongly suggests that the bells from Lamanai were made using the lost-wax casting technique.…”
Section: Finished Copper Objectsmentioning
confidence: 99%
“…El manejo del color mediante el dorado por oxidación presentó algunas diferencias entre los trabajadores metalúrgicos de la zona; en Panamá parece que la película superficial de óxido cuproso era disuelta por el ácido de carbonato de amonio presente en la orina (16) (29); del Ecuador aprendió el martillado y posterior recocido de los metales, y del área intermedia, el método de la cera perdida. En esta región abunda el cobre en forma de calcopirita, aunque también se presenta como malaquita, azurita y bornita, y el arsénico como arsenopirita; también hay yacimientos importantes de plata junto con latón, zinc y oro (30). De especial interés para el tema de este trabajo es la ausencia casi total de estaño, lo que impidió que se manufacturaran grandes cantidades de objetos de bronce estañoso.…”
Section: Característicasunclassified
“…Data for the Arteaga Complex and J-K arc assemblages are from Centeno- Garcia et al (1993), for the Zacatecas Formation from Centeno- Garcia and Silva-Romo (1997), for the Tejupilco metamorphic suite from Elias-Herrera et al (2003), for the Arperos Formation from Freydier et al (1996), and for IODP-DSDP 487-488 xi sediments from Verma (2000). Cumming et al (1979) and Hosler and Macfarlane (1996). The Pb growth curve of Stacey and Kramers (1975) Zartman and Doe (1981); the lead growth curve (SK) is from Stacey and Kramers (1975) Hemming and McLennan, 2001), and MORB-EPR (White et al, 1987) are also shown.…”
mentioning
confidence: 99%
“…Lead growth curve from Stacey and Kramers (1975) (Martiny et al, 1997;Martiny et al, 2000), and the Oaxaca (Martiny et al, 2000) terranes; the Texas "Grenville" (Smith et al, 1997;Cameron and Ward, 1998); the Santa Marta and Garzon Massifs (Colombia) and the Guichicovi Complex ; and the Olmos and Maranon Complexes (northern Peru) . SK represents the Stacey and Kramers (1975) Miranda-Gasca (1995), Hosler and Macfarlane (1996), and the present study; for Toluca metamorphic rocks from Martinez-Serrano et al (2004); for MORB-EPR from White et al (1987); for Pacific Ocean sediments (POS) from Hemming and McLennan (2001). The average upper crustal (UC) and orogene (OR) growth curves are from Zartman and Doe (1981); the lead growth curve (SK) is from Stacey and Kramers (1975) .5.…”
mentioning
confidence: 99%