鲁山茅店遗址与西土司式建筑传统的形成

IF 0.2 4区 历史学 0 ARCHAEOLOGY
Tianyi Wang
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引用次数: 0

摘要

摘要 先秦时代的大型庭院建筑群可分为两个系统:西土(中国西北部)类型和中原类型。前者以夯土建筑为特征,盛行于黄土高原;后者以瓦当技术著称,广泛分布于中原及周边地区。鲁山茅山的考古发现表明,西土家族院落建筑群的出现不晚于龙山时代晚期,并延续了近两千年。这两种制度都可能起源于仰韶晚期。西土型表明受到了华南地区的影响,而中原型则是由于气候、环境和资源的综合变化而形成的。院落建筑群在西周早期和晚期经历了两次大的转变,表明周人为保持其文化传统而采取的政治策略发生了重大变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Lushanmao site and the formation of the Xitu type architectural tradition
Abstract Large courtyard complexes in the pre-Qin times can be divided into two systems: the Xitu (northwest China) type and the Central Plains type. The former is characterized by the rammed earth construction and prevailed in the Loess Plateau; by contrast, the latter was well-known for the wattle-and-daub technology and widespread in the Central Plains and surrounding regions. The archaeological discoveries at Lushanmao suggest that the Xitu-type courtyard complexes were in use no later than the late Longshan period and lasted for nearly two thousand years. Both the two systems may have their origin in the late Yangshao period. The Xitu type indicates the influence of South China while the Central Plains type was formed due to a combination of the changes in climate, environment, and resources. Courtyard complexes underwent two major shifts during the early and late Western Zhou, suggesting the major changes in political strategies employed by the Zhou people to maintain their cultural traditions.
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来源期刊
Chinese Archaeology
Chinese Archaeology ARCHAEOLOGY-
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