Earth Science Frontiers ›› 2022, Vol. 29 ›› Issue (4): 330-344.DOI: 10.13745/j.esf.sf.2022.4.22
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FAN Chaoxi1(), XU Cheng1,2, CUI Ying1,*(
), WEI Chunwan1, KUANG Guangxi1, SHI Aiguo1, LI Zhuoqi1
Received:
2022-03-16
Revised:
2022-04-20
Online:
2022-07-25
Published:
2022-07-28
Contact:
CUI Ying
CLC Number:
FAN Chaoxi, XU Cheng, CUI Ying, WEI Chunwan, KUANG Guangxi, SHI Aiguo, LI Zhuoqi. Carbonatite magma and crustal metasomatism: A review[J]. Earth Science Frontiers, 2022, 29(4): 330-344.
研究区 | 地质背景 | 共生岩石组合 | 特征矿物 | 地球化学特征 |
---|---|---|---|---|
草滩 | 造山带 | 方解石碳酸岩、白云石碳酸岩、片麻岩 | 镁橄榄石 | 白云石碳酸岩比方解石碳酸岩具有更高的C同位素和更低Sr同位素组成 |
丰镇 | 造山带 | 花岗岩、辉石正长岩、碳酸岩 | 透辉石、钡冰长石 | 长石和辉石具有核边成分变化。碳酸岩和花岗岩有一致的Sr-Nd同位素特征 |
Kaiserstuhl | 大陆裂谷 | 碱玄岩、霞石岩、辉石岩、碳酸岩、正长岩 | 黑云母、透辉石 | 磷灰石具有核边成分变化,碳酸岩云母富Fe2+ |
Petyayan-Vara | 火成岩省 | 碳酸岩、高Ti碳酸岩、霓霞岩、辉石岩 | 板钛矿、透辉石、黑云母 | 主体的碳酸岩和接触带的高Ti碳酸岩具有不同C-O同位素组成 |
Nolans Bore | 火成岩省 | 麻粒岩、磷灰石脉 | 透辉石、榍石、钡冰长石 | 透辉石具有较高的(Lu/La)cn比值,相对于共生的榍石强烈富集Yb-Lu |
Table 1 Example characteristics of carbonatite reaction with the crust
研究区 | 地质背景 | 共生岩石组合 | 特征矿物 | 地球化学特征 |
---|---|---|---|---|
草滩 | 造山带 | 方解石碳酸岩、白云石碳酸岩、片麻岩 | 镁橄榄石 | 白云石碳酸岩比方解石碳酸岩具有更高的C同位素和更低Sr同位素组成 |
丰镇 | 造山带 | 花岗岩、辉石正长岩、碳酸岩 | 透辉石、钡冰长石 | 长石和辉石具有核边成分变化。碳酸岩和花岗岩有一致的Sr-Nd同位素特征 |
Kaiserstuhl | 大陆裂谷 | 碱玄岩、霞石岩、辉石岩、碳酸岩、正长岩 | 黑云母、透辉石 | 磷灰石具有核边成分变化,碳酸岩云母富Fe2+ |
Petyayan-Vara | 火成岩省 | 碳酸岩、高Ti碳酸岩、霓霞岩、辉石岩 | 板钛矿、透辉石、黑云母 | 主体的碳酸岩和接触带的高Ti碳酸岩具有不同C-O同位素组成 |
Nolans Bore | 火成岩省 | 麻粒岩、磷灰石脉 | 透辉石、榍石、钡冰长石 | 透辉石具有较高的(Lu/La)cn比值,相对于共生的榍石强烈富集Yb-Lu |
Fig.4 Schematic representation of the reaction between carbonatite and crust and associated REE mineralization event based on recent experimental simulations. Modified after [28].
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