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New Sub-Himalayan Holocene Lithic Industry

机译:新亚马拉雅大全新世岩石行业

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The Palaeolithic investigations in the northwestern sub-Himalayas have since been known by the Soanian industries first discovered by de-Terra and Paterson (1939) in the Potwar region of Pakistan. After independence, the research in this region was carried out mainly by Paterson & Drumond (1962) and later by Rendell et al (1989), Dennell et al (1991) and Salim (1994) in Pakistan, by Lal (1956), Sankalia, (1974,) Mohapatra (1990, 2007), Mohapatra& Singh (1979) Saroj (1974), Sankhyan (1983), Karir (1985), Joshi (1968), Singh & Karir (1998) and Gaillard et al (2008), and then recently by Chauhan (2004, 2007a, 2007b) and Soni & Soni (2005, 2007, 2008, 2009), in India. The lithic artefacts that have since been collected by most of the earlier investigators were claimed as belonging to the Mode-1 category and have generally followed the approach of de-Terra & Paterson though the recent finds (Chauhan 2004, Soni& Soni 2008,2009) scientifically deem to prove something entirely different. The earlier investigators (particularly in the Indian part of the sub-Himalayas) never found any lithic industry in stratigraphic or datable context and they had merely speculated (Mohapatra 2007) the Soanian to have existed probably from mid to late or terminal Pleistocene. Most of the earlier researchers had categorized Soanian either on the basis of now out-dated Alpine glaciations chronology (de-Terra & Paterson 1939) or the tool typology and other un-datable geological attributes. However, the present authors' discovery of Soanian artefacts along with terracotta pieces and some new tool types strongly demands that the stone-age research in the northwestern sub-Himalayas be reconsidered in light of these new revelations. In the following, three already reported and one new site are (Fig.1) being discussed which call for a change in the interpretation of the Soanian and its relation to the Holocene epoch geo-archaeology.
机译:西北部喜马拉雅山的古石调查以来,Soanian Industries发表于De-Terra和Paterson(1939)在巴基斯坦的波尔瓦地区发现。独立后,该地区的研究主要由Paterson&Charmond(1962),后来通过Rendell等人(1989),Dennell等人(1991)和Sanc(1956),Sankala(1956)的Salim(1994) ,(1974,)Mohapatra(1990,2007),Mohapatra&Singh(1979)Saroj(1974),Sankhyan(1983),Karir(1985),Joshi(1968),Singh&Karir(1998)和Gaillard等人(2008)然后,最近在Chauhan(2004年,2007A,2007B)和Soni&Soni(2005,2007,2008,2009),在印度。由于大多数早期调查人员收集的岩石人工制品被声称属于模式-1类,并且虽然最近的发现(Chauhan 2004,Soni&Soni 2008,2009),虽然虽然是德拉瓦和帕特森的方法科学地认为完全不同的东西。早期的调查人员(特别是在亚马拉雅州的印度部分)中从未发现过地层或可婚环境中的任何岩石行业,他们只是推测(Mohapatra 2007)索尼安可能从中期到后期或终端全文中存在。早期的大多数研究人员都在现在的外国过期的高山冰川冰川时间(De-Terra&Paterson 1939)或工具类型和其他未经数据的地质属性的基础上分类了Soanian。然而,本作者对索拉尼亚人工制品的发现以及赤土陶器件以及一些新的工具类型强烈要求,鉴于这些新的启示,西北大喜马拉雅山的石头龄研究是重新考虑的。在下文中,已经报告了三个,并讨论了一个新的网站(图1),讨论了哪个新网站,该网站呼吁改变索南人及其与全新世纪时期地理学的关系。

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