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Petrographyc studies from mayan ceramics, Late Classic (600-900 a.d.), Chinikiha, Chiapas, Mexico

机译:墨西哥恰帕斯州奇尼基哈的玛雅陶瓷岩石学研究,晚期经典(公元600-900年)

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Chinikiha is a Maya archaeology place from Classic period (250-900 a.D.); it is located in Chiapas and Tabasco States, Mexico. Chinikiha has at least 120 monumental structures, palace type and pyramidal structures. The petrography studies of 21 ceramic samples, shows: a) Siliciclastic pastes (with 45,5- 84,5% matrix, the average is 69,19%) and b) carbonated pastes (with 18-64% matrix, carbonate 79%, the average 30,5%). The carbonated pastes has grain support but the silicoclastic pastes has matrix support. The earliest Mayan-ceramic pastes are carbonates compounds but later, they were changed by siliciclastic compounds. The technologyc changes probably occurred when the Mayan decided to change the carbonated pastas by siliciclastic pastes.The Chinikihá pots, are 80% made using siliciclastic pastes, with mica. The ceramic-fire temperature probably did not reach 950°C, instead the carbonated pastes probably did not 800°C. If the raw material was not imported, probably the rock source coming from Eocene sandstones or lutites rocks or Miocene sandstones or both. Furthermore, the volcanic shards found in the thin sections, possible coming from volcanic soils, for instance, Chichon volcano-tuffs deposits. Some pastes shows the diatoms fossils. The raw source, probably, come from fresh water lakes.
机译:Chinikiha是古典时期(公元250-900年)的玛雅考古学场所;它位于墨西哥恰帕斯州和塔巴斯科州。 Chinikiha至少有120座纪念性建筑,宫殿式和金字塔式建筑。对21个陶瓷样品的岩石学研究表明:a)硅质碎屑(基质为45,5-84.5%,平均值为69.19%),b)碳酸盐化糊状物(为18-64%,碳酸盐为79% ,平均30.5%)。碳酸化的糊状物具有谷粒支持,而硅碎屑糊状物具有基质支持。最早的玛雅陶瓷浆料是碳酸盐化合物,但后来被硅弹性化合物改变了。当玛雅人决定通过硅质碎屑改变碳酸面食时,技术发生了变化。Chinikihá花盆80%是用硅质碎屑和云母制成的。陶瓷火的温度可能未达到950°C,而碳酸浆则未达到800°C。如果未进口原材料,则岩石来源可能来自始新世砂岩或黄铁矿岩石或中新世砂岩或两者。此外,在薄壁部分发现的火山碎屑可能来自火山土壤,例如Chichon火山凝灰岩沉积物。一些糊状物显示了硅藻化石。原始来源可能来自淡水湖泊。

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