从较重的矿物中分离牙形石元素的新技术

IF 1.2 4区 地球科学 Q3 PALEONTOLOGY
L. Jeppsson, Rikard Anehus
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引用次数: 36

摘要

牙形石元素密度在2.90 ~ 3.04 g cm-3之间,可能非常接近3.00。在密度分离之前去除所有白云石和碳酸钙的痕迹,使多钨酸钠溶液的粘度足够低,使其可用于高达3.04 g cm-3的密度分离。在大多数情况下,通过将该方法添加到现有的标准技术中,可以产生几乎干净的磷酸馏分。并对氧化法脱除黄铁矿的工艺进行了探讨。在各种物理浓缩工作中,考虑“堆积密度”对于取得好的结果是非常重要的,特别是对于一致性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A new technique to separate conodont elements from heavier minerals
The density of conodont elements is between 2.90 g cm-3 and 3.04 g cm-3, probably very close to 3.00. Removing all traces of dolomite and calcium carbonate before density separation keeps the viscosity of sodium polytungstate solution low enough to make it useful for density separations as high as 3.04 g cm-3. In most cases, a nearly clean phosphatic fraction can be produced by adding this method to existing standard techniques. The oxidizing technique to remove pyrite is also discussed. In all kinds of physical concentration work consideration of the “bulk density” is very important for good results, especially regarding coniforms.
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来源期刊
Alcheringa
Alcheringa 地学-古生物学
CiteScore
2.60
自引率
7.70%
发文量
28
审稿时长
>12 weeks
期刊介绍: Alcheringa : An Australasian Journal of Palaeontology is the official journal of the Australasian Palaeontologists. Alcheringa covers all aspects of palaeontology and its ramifications into the earth and biological sciences, including: Taxonomy- Biostratigraphy- Micropalaeontology- Vertebrate palaeontology- Palaeobotany- Palynology- Palaeobiology- Palaeoanatomy- Palaeoecology- Biostratinomy- Biogeography- Chronobiology- Biogeochemistry- Palichnology. Review articles are welcome, and may be solicited from time to time. Thematic issues are also possible. Emphasis is placed on high quality and informative illustration, in both line drawings and photographs. Papers of general significance may receive preference over those of more local interest.
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