Recommendations for Kübler Index standardization
Recommendations for Kübler Index standardization
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DOI：
10.1180/claymin.2015.050.3.02
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发表时间：
2015-08
期刊：
影响因子：
1.5
通讯作者：
L. Warr;R. F. Mählmann
中科院分区：
文献类型：
--
作者：
L. Warr;R. F. Mählmann
摘要经过2014年德累斯顿中欧粘土会议的圆桌讨论，伊利石“结晶度”Kübler指数标准化的新建议已达成一致。将继续使用岩石碎片样品形式的结晶度指数标准，以及Warr&Rice(1994)提出的相同数值标度。然而，为了与Kübler(1967)Anchizone的原始工作定义一致，结晶度指数标准(CIS)的上下限从0.25°2θ和0.42°2θ适当调整为0.32°2θ和0.52°2θ。这一调整是基于巴塞尔实验室、诺沙特尔实验室和独联体实验室之间的实验室间相互关系。这一修正的细节载于第一份说明，正如圆桌会议上讨论的那样，并将通过独联体和前库布勒-弗雷-基施标准之间的关联计划进一步得到证实。
Abstract Following a round-table discussion at the Mid-European Clay Conference in Dresden 2014, new recommendations for illite ‘crystallinity’ Kübler index standardization have been agreed upon. The use of Crystallinity Index standards in the form of rock-fragment samples will be continued, along with the same numerical scale of measurement presented by Warr & Rice (1994). However, in order to be compatible with the original working definition of Kübler’s (1967) anchizone, the upper and lower boundary limits of the Crystallinity Index Standard (CIS) scale are adjusted appropriately from 0.25°2θ and 0.42°2θ to 0.32°2θ and 0.52°2θ. This adjustment is based on an inter-laboratory correlation between the laboratories of Basel, Neuchâtel and the CIS scale. The details of this correction are presented in this first note, as discussed at the round-table meeting and will be further substantiated by a correlation program between CIS and former Kübler-Frey-Kisch standards.