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Intrasource Chemical Variability and Secondary Depositional Processes · Study

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ChapterIntrasource Chemical Variability and Secondary Depositional Processes

Michael Steven Shackley1998

Chapter1998

Intrasource Chemical Variability and Secondary Depositional Processes

Michael Steven Shackley

31 citations·0/0 files stored·Springer eBooks

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Cultural Heritage Materials Analysis Mineralogy and Gemology Studies Archaeology and ancient environmental studies

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Citations in this library

Stored only when both papers are in the corpus — 31 citations exist upstream.

References

1992Chemical characterization of ceramic pastes in archaeology 1977ALTERNATIVE MODELS FOR EXCHANGE AND SPATIAL DISTRIBUTION 2009Exchange Systems in Prehistory 1988Sources of Archaeological Obsidian in the Southwest: An Archaeological, Petrological, and Geochemical Study 1993Archaeology, geology, and geochemistry in obsidian provenance studies 1982Contexts for Prehistoric Exchange 1987Archaeometry : further Australasian studies 1995Sources of Archaeological Obsidian in the Greater American Southwest: An Update and Quantitative Analysis

Cited by

2009How reliable are our published archaeometric analyses? Effects of analytical techniques through time on the elemental analysis of obsidians 2002Quantitative EDXRF Studies of Obsidian Sources in Northern Hokkaido 2008Source selectivity: An assessment of volcanic glass sources in the southern primorye region, far East Russia 2012New pieces: the acquisition and distribution of volcanic glass sources in northeast China during the Holocene 2015Reassessing obsidian field relationships at Glass Buttes, Oregon 2017Elemental, isotopic, and geochronological variability in Mogollon‐Datil volcanic province archaeological obsidian, southwestern USA: Solving issues of intersource discrimination

Details

Year1998

Typechapter

Published1998-01-01

VenueSpringer eBooks

Languageen

Citations31

Files0 public / 0

ShelfCultural Heritage Materials Analysis

Identifiers

doi10.1007/978-1-4757-9276-8_4

openalex_workW70065167

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