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Archaeological formation theory and geoarchaeology: State-of-the-art in 2016

机译:考古学形成理论与地理学论:2016年最先进的

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Since the influential work of Michael B. Schiffer on formation processes has been published in 1987, much has advanced on the part of environmental formation processes also known as N-transforms. Most new knowledge is the result of research conducted by geoarchaeologists. On the theoretical level, a huge leap forward was made with the realization that occupation deposits are artifacts of human activity. The focus of formation theory thus shifted from the artifact to the deposit. Methodological innovations and a geoarchaeological tool-kit, notably including the contextual technique of micromorphology, followed. Empirical studies of archaeological occupation deposits contributed new spatial and stratigraphic knowledge and understanding. A holistic middle-range methodology termed geo-ethnoarchaeology was developed, whereby macroscopic and microscopic artifacts are studied together with their associated sediments in ethnographic contexts, providing contextual (social) information about the relationship between artifacts and the surrounding sediments as archaeological assemblages form. This method is especially powerful when sequentially dated abandoned settlements or features are studied to provide mechanistic understanding of assemblage and/or site formation through degradation. Because geoethnoarchaeology is based on general chemical, biological and physical laws, the resultant mechanistic models are applicable globally, for any time period, culture, and environment. The new tools and mechanistic understanding by which N-transforms are currently studied, provide means to more reliably interpret the archaeological record, which is crucial for the credibility of archaeology. Therefore, when studying archaeological assemblages one should utilize the tool-kit developed by geoarchaeologists to first assess the states of preservation of the various material assemblages (macroscopic and microscopic), as it should be borne in mind that assemblages identified to be well-preserved will produce the most reliable archaeological interpretation. The theory and method of geoarchaeology have matured enough to allow responsible archaeological research into the meaning of spatial and temporal (stratigraphic) patterns at any given site. (C) 2017 Elsevier Ltd. All rights reserved.
机译:自1987年迈克尔·B·希弗(Michael B.Schiffer)关于形成过程的有影响力的研究发表以来,在环境形成过程(也称为N-变换)方面取得了很大进展。大多数新知识都是地质考古学家研究的结果。在理论层面上,随着人们认识到占领矿床是人类活动的产物,取得了巨大的飞跃。因此,地层理论的重点从人工制品转移到矿床。随后是方法创新和地质考古工具包,尤其是微形态的上下文技术。考古占领矿床的实证研究提供了新的空间和地层学知识和理解。发展了一种被称为“地质民族考古学”的整体中期方法,通过该方法,在民族志背景下研究宏观和微观文物及其相关沉积物,提供有关文物与周围沉积物之间关系的背景(社会)信息,以形成考古组合。当研究顺序年代的废弃定居点或特征,以提供通过退化的组合和/或场地形成的机械理解时,这种方法尤其有效。由于地球人种进化论是基于一般的化学、生物和物理定律,因此产生的力学模型适用于全球任何时间段、文化和环境。目前研究N-变换的新工具和机械理解为更可靠地解释考古记录提供了手段,这对考古学的可信度至关重要。因此,在研究考古组合时,应使用地质考古学家开发的工具包,首先评估各种材料组合(宏观和微观)的保存状态,因为应记住,被确定为保存完好的组合将产生最可靠的考古解释。地质考古学的理论和方法已经足够成熟,可以对任何特定地点的时空(地层)模式进行负责任的考古学研究。(C) 2017爱思唯尔有限公司版权所有。

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