دورية أكاديمية

Do Pegmatites Crystallise Fast? A Perspective from Petrologically-Constrained Isotopic Dating

التفاصيل البيبلوغرافية
العنوان: Do Pegmatites Crystallise Fast? A Perspective from Petrologically-Constrained Isotopic Dating
المؤلفون: Daniil V. Popov
المصدر: Geosciences, Vol 13, Iss 10, p 297 (2023)
بيانات النشر: MDPI AG, 2023.
سنة النشر: 2023
المجموعة: LCC:Geology
مصطلحات موضوعية: pegmatite, rate of crystallisation, geochronology, Geology, QE1-996.5
الوصف: Most recent studies consider the formation of individual pegmatite bodies to be a fast process with estimated crystal growth rates reaching a walloping 10 m/day. This opinion is presumably underpinned by the traditional way of thinking of them as the end products of magmatic fractionation. Indeed, modelling has shown that if a pegmatite-forming substance with a temperature near granitic solidus intrudes into a much colder host rock, as recorded in some outcrops, it must cool rapidly. From here, a conclusion is made that the crystallisation must likewise be rapid. However, this view is challenged by several studies that published isotopic dates supported by petrological characterisation of the analysed materials, which suggested or can be used to suggest that some minerals in pegmatites grew over millions of years. Surprisingly, such in-depth work on the geochronology of individual pegmatite bodies is relatively uncommon, so it is early to make generalisations. Here, I highlight some of the existing evidence with the aim to stimulate further research into the timescales of pegmatite crystallisation, including the use of petrologically constrained isotopic dating.
نوع الوثيقة: article
وصف الملف: electronic resource
اللغة: English
تدمد: 13100297
2076-3263
Relation: https://www.mdpi.com/2076-3263/13/10/297; https://doaj.org/toc/2076-3263
DOI: 10.3390/geosciences13100297
URL الوصول: https://doaj.org/article/c7441ef0d7aa45979d28dbce6854e221
رقم الأكسشن: edsdoj.7441ef0d7aa45979d28dbce6854e221
قاعدة البيانات: Directory of Open Access Journals
الوصف
تدمد:13100297
20763263
DOI:10.3390/geosciences13100297