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, altered feldspar, transformed into aggregate of clay minerals; Bt: biotite; Chl: chlorite
, Schematic cross-section of the Cambrian meta-sediments to the south of Jinggangshan, location on Fig
, sense of shear in high grade rocks; (3) sense of shear assigned to an inherited structure or a late phase; (4) sense of shear in Sinian?Ordovician meta-sediments; (5) cleavage-foliation dip; (6) sample location for dating; (7) location of dating result from the literature (Ar: Ar?Ar method; K?Ar: K?Ar method; bi: biotite; ms: muscovite; mo: U?Th?Pb EPMA method on monazite) Data sources, p.and, 1997.
, Jianyang cross-section, location on Fig. 7. The arrows show the lineation direction and the determined sense of shear
, Jian'ou); note some sigmoids indicating a southward shearing. (b) Same locality, closer view of another outcrop oriented SSW?NNE; note the meta-pillow (upper left corner) and some sigmoids (picture centre above the hammer) indicating a southward shearing. (c) WU-072, photomicrograph of the Jian'ou amphibole schist, asymmetric amphiboles around feldspar porphyroclast, top-to- N130 sense of shear, PPL. (d) WU-473, amphibole schist, Jian'ou, shear bands and sigmoids indicating a top-to-SE sense of shear meta-basic greenschist, asymmetric feldspar porphyroclast indicating a top-to-N210 sense of shear Am: amphibole; Fsp: feldspar, CPL. (e) WU-061 PPL. (f) Outcrop view of the Huaquan gabbro
, Photomicrographs of meta-siliceous rocks sericite quartzite, incipient dynamic quartz recrystallization by bulging (BLG), shearing toward N190, CPL. (b) WU-100, between Qitou and Shaowu, quartz schist mylonite, note the sub-grains and the birth of small quartz crystals by bulging, fabric toward the south, CPL. (c) WU-067, S of Zhenghe, bedded quartzite (metachert), strong dynamic quartz recrystallization by bulging, the fabric indicates a top-to-N200 (left) sense of shear, CPL. (d) WU-046, Yekeng bridge (Longbeixi area), muscovite quartzite, dynamic recrystallization by sub-grain rotation, shearing toward N190 (left), CPL. (e) WU-041, Longbeixi, siliceous marble, quartz recrystallization by SGR and BLG, fabric toward the south, CPL. (f) WU-049, near Xiazhuang (Longbeixi area), quartzite mylonite, dynamic quartz recrystallization by SGR, fabric toward the south, CPL. (g) WU-042, Longbeixi, quartz muscovite schist, asymmetric muscovite pressure shadows around quartz porphyroclasts, top-to-N160 sense of shear Ms: muscovite; Py: pyrite; Qtz: quartz
, Cross-sections of mafic?ultramafic rocks-bearing thrust sheets, location on [Fig. 1] and [Fig. 7]. (a) Chencai cross-section, modified after Charvet et al. (1999) and Shui et al. (1988)and (b) Hudiejie cross-section, 2009.
, Yongping and Beili cross-sections, location on Fig. 7. (a) Beili section and (b) Yongping section
, Geochronological data. Results of sample WU-227-JC01. Photomicrographs, BSE images and Th
, Geochronological data. Results of sample WU-816-JC02; (a?c) Th/Pb vs. U/Pb diagram Photomicrographs and BSE images for A, B and hybrid population
, Geodynamic evolutionary model. (a) around 850 Ma, rifting stage; (b) around 460 Ma, compressional stage, piling of nappes and prograde metamorphism, pp.440-430
, AM: asthenospheric mantle; LM: lithospheric mantle; LC: lower crust; UC: upper crust, J: Jinggangshan; N: Ninghua; Na: Nanping