[R8-04]Coalescing detrital zircon geochronology and litho-structural mapping in identification of MBT in Himachal Himalayas
*Sarkar Dyuti Prakash1、Ando Jun-ichi1、Das Kaushik1、Ghosh Gautam2(1. Hiroshima Uni.、2. Presidency Uni.)
キーワード:
MBT、U-Pb geochronology、Calcite e-twins
Elucidating deformation mechanisms and fault behavior require identification of the fault contact. However, discerning exact fault boundary can be a challenge in cases where lithology is similar, or fault rocks are not preserved. In current study we consider a inferred part of MBT and combining U-Pb detrital geochronology and litho-structural mapping we identify the exact fault boundary of MBT in the study area.
