������( Larap) ����ͭ��󴲲��ڷ��ɱ���鸩�����ε�����½Ե�ĵ�����ɽ���ϣ����ڷ��ɱ������߻����Ѵ����ԡ������λ�ڹŽ��ͽ���������ʴ�䰲ɽ�ҡ������Һ͹���ͳ�Ľ��ҡ����һ�ҳ�ҵ�����ǶȲ��������׷�ٶ��Ѵ��ϡ�������İ�ɽ�ҡ������ҵ���ɫ���ʹ�״չ���Ļ���ɫ��Һ����ʴ����ϵ���������ʴ����У����Ʋ�״��͸��״; ���������ϲ���λ��ͭ��������������²�����ƶ������������; ���������ͭ���⣬ͭ������ְ��������������ܵȣ���ʯ�еĽ��������Դ�����Ϊ��������л����󡢻�ͭ�󡢻���󡢴Ż����������˿����Ȼ��ȡ�Ԫ����ϳ�����ͭ�����⣬���н������ܺ��˵ȣ������ƥ�˰ӡ�Candelaria ( ����) ����������( IOCG) ͭ�����ȣ������տ󴲳���������������ͭ���������͡�

Larap iron-copper-molybdenum deposit is formed in the island arc orogen of Luzon passive continental margin which is subducted by Philippine Plate��and located near Philippines central strike-slip fracture zone�� The mineral-bearing layer is situated on tracing fracture zone of outpouring angular uncomformity between altered andesite and breccia in upper Oligocene and hornfel and hornfel shale in Paleogene�� Large area of faded andesite and hornfel and zonal distributed grey-green hydrothermal fluid are metasomatized with altered rock series��the orebody is formed in such alteration zone with laminiplantation and lense shapes�� Iron orebody is located in upper layer�� while the copper-molybdenum ore body is located in lower layer of iron orebody together with lean magnetite�� The iron orebody associates with copper and molybdenum��the copper-molybdenum body associates with iron��gold�� silver��cobalt and others�� Magnetite is the dominant metallic mineral in the ore��secondly are pyrite��chalcopyrite�� molybdenite��pyrrhotite��uraninite��nature gold and so on�� Besides iron��copper and molybdenum��other element combinations include gold��silver��cobalt and uranium�� Compared with Olympic dam and Candelaria ( Chile) ironoxide copper-gold deposits��Larap deposit belongs to a new type of iron oxide copper-molybdenum-gold deposit��