; M. This may be possible by observing porphyroblast formation in cleavages of known deformation age, by identifying metamorphic mineral assemblages created by different events, or via geochronology. Intersection lineations in rocks, as they are the product of the intersection of two planar structures, are named according to the two planar structures from which they are formed. For instance, the intersection lineation of a S cleavage and bedding is the L intersection lineation (also known as the cleavage-bedding lineation).
ครับท่าน เรือบาว์นติฟุล มาจาก พลิเมาท์scb_mt_enth_2020 scb_mt_enth_2020