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Progress in Earth and Planetary Science
Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: Carbonate clumped isotope thermometry of fault rocks and its possibilities: tectonic implications from calcites within Himalayan Frontal Fold-Thrust Belt

Fig. 2

a The gouge rocks of NT exhibiting fragmented calcite veins (PJ5). The inset shows fragments of calcite vein (arrow) in obtained sample. b Folded calcite veins (arrow) (PWN1) occurring in the hanging wall of BT. c Co-folded calcite veins (CM2) occurring near a splay thrust of RT. d Folded calcite veins (KP1) occurring near deformed rocks of RT. e Calcite veins (arrows) within fossiliferous limestones of Subathu Formation in footwall of MBT. f Folded and deformed calcite veins (long arrows) (GM8) within the calcareous shale and limestone alternation of Subathu Formation occurring in footwall of MBT. The narrow dilational veins (short arrow) (GM8a) are of older generation. g Fossiliferous limestone of Subathu formation (CM1) showing well preserved fossils (arrows). h Stromatolitic limestone (GM5I) (arrows show lining of stromatolite layers) of Krol Formation, occurs as discrete bodies within the hanging wall of MBT

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