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从泰米尔纳德邦阿蒂拉帕卡姆旧石器时代考古遗址采集的岩石样本中石英的矿物质和结晶度指数数据。

Data on minerals and crystallinity index of quartz in rock samples collected from Paleolithic archaeological site of Attirampakkam, Tamil Nadu.

作者信息

Tamilarasi A, Sathish V, Manigandan S, Chandrasekaran A

机构信息

Sri Sivasubramaniya Nadar College of Engineering (Autonomous), Chennai, Tamilnadu 603110, India.

出版信息

Data Brief. 2021 Nov 13;39:107571. doi: 10.1016/j.dib.2021.107571. eCollection 2021 Dec.

Abstract

In the present work, rock samples were collected from Paleolithic archaeological site of Attirampakkam, Tamil Nadu, India to assess the mineralogical composition using Fourier transform infrared-spectroscopic (FT-IR) technique and X-Ray Diffraction Spectrometry (XRD). The quartz, kaolinite, montmorillonite, calcite, orthoclase, microcline and illite minerals are identified in rock samples and crystallinity index of quartz (SiO) is estimated for all the samples by comparing the ratio of intensity of the characteristic peak at 778 and 695 cm using FT-IR spectrum. In rock samples, calculated crystallinity index of quartz is greater than the 1 from FT-IR spectrum and it shows that the distribution is disordered in nature. Additionally, some more minerals such as hematite and rutile are identified in rock samples by X-ray diffraction technique. This extensive study shows that archeological rock samples are wide variation in mineral composition.

摘要

在本研究中,从印度泰米尔纳德邦阿蒂拉姆帕卡姆的旧石器时代考古遗址采集了岩石样本,以使用傅里叶变换红外光谱(FT-IR)技术和X射线衍射光谱(XRD)评估矿物成分。在岩石样本中鉴定出了石英、高岭石、蒙脱石、方解石、正长石、微斜长石和伊利石矿物,并通过使用FT-IR光谱比较778和695 cm处特征峰的强度比,估算了所有样本中石英(SiO)的结晶度指数。在岩石样本中,通过FT-IR光谱计算出的石英结晶度指数大于1,这表明其分布本质上是无序的。此外,通过X射线衍射技术在岩石样本中鉴定出了一些其他矿物,如赤铁矿和金红石。这项广泛的研究表明,考古岩石样本的矿物成分存在广泛差异。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/10fc/8605056/bf5849cc548e/gr1.jpg

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