Drill site J10 for the planned follow-up drilling at New Boston, some 500 m east of NB26-003. Polyphase stockwork quartz veins occur in Triassic limestone completely recrystalized to marbel, with pervasive, dark red-brown, garnet-rich skarn alteration and replacement. Evident are vein offset and vein- internal extensional cracks with mineralization in polyphase vein history.
Drill site J10 for the planned follow-up drilling at New Boston, some 500 m east of NB26-003. Polyphase stockwork quartz veins occur in Triassic limestone completely recrystalized to marbel, with pervasive, dark red-brown, garnet-rich skarn alteration and replacement. Evident are vein offset and vein- internal extensional cracks with mineralization in polyphase vein history.