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首页> 外文期刊>Lithos: An International Journal of Mineralogy, Petrology, and Geochemistry >Duration and periodicity of kimberlite volcanic activity in the Lac de Gras kimberlite field, Canada and some recommendations for kimberlite geochronology
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Duration and periodicity of kimberlite volcanic activity in the Lac de Gras kimberlite field, Canada and some recommendations for kimberlite geochronology

机译:加拿大Lac de Gras金伯利岩田中金伯利岩火山活动的持续时间和周期性,以及对金伯利岩年代学的一些建议

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Establishing the emplacement ages and distribution pattern of Central Slave kimberlites has played a key role in diamond exploration within the Lac de Gras kimberlite field. Nonetheless, emplacement age information is lacking for approximately 80% of the known kimberlites in this field making the assessment of emplacement age patterns difficult. This study expands the number and geographic coverage of kimberlite emplacement ages within the Lac de Gras field to re-assess the absolute timing, duration, and possible number of pulses of kimberlite eruption. U-Pb perovskite ages for eight previously undated kimberlites and an additional thirteen kimberlites, which were previously dated by either the Rb-Sr or U-Pb methods, fall within the age range of 75-45 Ma, as previously suggested for kimberlite magmatism in this area. We report the first Carboniferous age kimberlite in the Central Lac de Gras field - the Eddie kimberlite - with a U-Pb perovskite age of 321.0 +/- 3.0 Ma. A compilation of 57 kimberlite emplacement ages from the central Lac de Gras field was evaluated using probability density and mixture modeling methods. Five short-duration (4-5 Ma) periods of kimberlite magmatism are recognized at 48, 54, 61, 66 and 72 Ma; the three younger pulses have been previously recognized and remain relatively unchanged. The 54 Ma pulse represents the major kimberlite eruption event containing similar to 40% of the currently dated kimberlites in Lac de Gras field. A detailed evaluation of the temporal-spatial evolution of Lac de Gras kimberlites reveals that the oldest diamond-poor kimberlites (75-60 Ma) were emplaced in the northern and eastern parts of the field whereas the younger (55-48 Ma) economic kimberlites are concentrated in the center of the field. (C) 2015 Elsevier B.V. All rights reserved.
机译:建立中央奴隶金伯利岩的进驻年龄和分布模式在Lac de Gras金伯利岩领域的钻石勘探中发挥了关键作用。但是,该领域中约80%的已知金伯利岩都缺乏进位年龄信息,因此很难评估进位年龄模式。这项研究扩大了Lac de Gras油田内金伯利岩侵袭年龄的数量和地理覆盖范围,以重新评估金伯利岩喷发的绝对时间,持续时间和可能的脉冲数。如之前对金伯利岩岩浆作用的建议,年龄范围为75-45 Ma的U-Pb钙钛矿年龄介于75-45 Ma之间。这片区域。我们报告了中部Lac de Gras油田中的第一个石炭纪金伯利岩-埃迪金伯利岩-U-Pb钙钛矿年龄为321.0 +/- 3.0 Ma。使用概率密度和混合建模方法评估了Lac de Gras中心地区57个金伯利岩的侵袭年龄。在48 Ma,54 Ma,61 Ma,66 Ma和72 Ma上,金伯利岩岩浆作用有5个短时期(4-5 Ma)。先前已识别出三个年轻脉冲,并保持相对不变。 54 Ma脉冲代表了主要的金伯利岩喷发事件,其中约40%的Lac de Gras田地中的日期已过期的金伯利岩发生了。对Lac de Gras金伯利岩的时空演变的详细评估表明,最贫金刚石的金伯利岩(75-60 Ma)分布在该油田的北部和东部,而较年轻的经济金伯利岩(55-48 Ma)集中在领域的中心。 (C)2015 Elsevier B.V.保留所有权利。

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