About Lüliang rock
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3 FAQs about [Lüliang rock]
What type of rocks are found in Lüliang group?
The Lüliang Group consists mainly of greenschist-amphibolite facies metasedimentary assemblages with banded iron formation (BIF) in the lower part and bimodal volcanic rocks in its upper part [Liu et al., 2011].
What type of metamorphism did the Lüliang complex experience?
Combined with the metamorphic characteristics of other regions in the Lüliang Complex, it can be inferred that the Lüliang Complex has experienced medium-pressure facies series metamorphism, with greenschist to amphibolite facies in the middle and amphibolite to granulite facies in the northwest and southeast.
Which dykes are dominant in the Lüliang area?
Three trends (E-W, NW-SE, and NE-SW) were identified in the Lüliang area. Among these, the E-W trending mafic dykes are dominant. The dykes are vertical to subvertical, and in sharp contact with the country rocks and have chilled margins. These dykes are typically 15–50 m in width, and up to 10–15 km in length.