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《Journal of Jiling University (Earth Science Edition)》 1985-02
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Sun Chao (Changchun Academy of Geology)  
\s a gross lincation in strongly deformed rocks, the mullion structure has got more and more attention.In articles they are commonly described as a lineation related to the fold structure, and generally, considered to be b-axis structure.Mullion structures related to the compression zone are different from the above-mentioned ones. They are found in existence by the side of and inside the compression zone, their axes run parallel to the extension of the compression zone. Thus, it can be used as an important criterion to identify the existence of compression-fracture zones or compression structures.
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