▁range ▁during ▁its ▁u pl ift . ▁These ▁sed iment ary ▁rocks ▁have ▁been ▁highly ▁de formed ▁by ▁the ▁continued ▁u pl ift ▁of ▁the ▁H imal aya . ▁The ▁upper ▁Pro ter oz o ic ▁to ▁lower ▁Camb rian ▁L esser ▁H imal aya ▁sed iment ary ▁rocks ▁represent ▁the ▁H imal aya ' s ▁main ▁range ▁front . ▁These ▁rocks ▁are ▁often ▁thr usted ▁over ▁the ▁all uv ial ▁rocks ▁of ▁the ▁sub - H imal aya . ▁The ▁L esser ▁H imal aya ▁also ▁contains ▁gran ites ▁and ▁f els ic ▁vol can ic ▁rocks . ▁The ▁Central ▁H imal ay an ▁Domain ▁contains ▁rocks ▁from ▁the ▁T eth ys ▁Ocean ▁and ▁is ▁also ▁intr ud ed ▁by ▁Mi oc ene ▁gran ites , ▁related ▁to ▁the ▁formation ▁of ▁the ▁H imal aya . ▁The ▁Ind us ▁S uture ▁Zone ▁is ▁the ▁s uture ▁zone ▁with ▁the ▁L has a ▁ter rane ▁to ▁the ▁North . ▁It ▁contains ▁the ▁o phi ol ites ▁and ▁island ▁arc ▁related ▁ igne ous ▁rocks ▁mostly ▁from ▁the ▁Mes oz o ic . ▁ ▁Q ili ans han ▁O ro gen ▁ ▁The ▁Q ili ans han ▁O ro gen ▁( also ▁Q ilian ▁Sh an ▁O ro gen ) ▁formed ▁in ▁the ▁Early ▁to ▁Mid ▁Pale oz o ic ▁in ▁modern ▁North ▁West ▁China . ▁The ▁rocks ▁of ▁the ▁region ▁record ▁a ▁Camb rian ▁to ▁Dev onian ▁sub du ction ▁acc ret ion ▁complex . ▁ ▁Central ▁Asian ▁Or igen ic ▁B elt