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Welcome to Jabal Corporate Entity Website

Jabal Grassroot Central Mindanao based corporate entity focused in polymetallic exploration notably, Copper, Zinc, Gold, Silver, Cobalt, Molybdenum, and other based metals Lead, Nickel, Manganese, Chromite, etc.

Excerpt from JORC Complying Competent Person’s Report done by Robert Mclean, Senior Consultant Geologist, CSA-Australia Pty. Ltd, showed High Prospective Economic Scale VMS Mineralization Highlights.

Furthermore, JORC Complying Petrographic Study of Ten Rock Samples taken from Jabal tenement done by Mr. Douglas Mason, Petrological Services for the Mineral Exploration and Mining Industry, Mason Geosciences Pty Ltd, Adelaide, Australia stated that most of the samples collected under study belong to two rock groups: altered andesitic volcanogenic rocks and fine-grained massive sulphide rocks. Together, these rocks are considered to represent a volcanic-hosted massive sulphide (VMS or VHMS) environment.

Recent geological investigation entitled “BRECCIA-HOSTED VOLCANOGENIC MASSIVE SULFIDE DEPOSIT AT JABAL MINING CLAIMS, NORTH COTABATO MINDANAO ISLAND, PHILIPPINES, done by Jose D. Madrona ABSTRACT stated:

The lithological units at Jabal Development Mining, Inc. tenement are associated with ultramafic composition and mafic rock of massive lavas, pillow lavas and volcaniclastic sediments of the dismembered ophiolite. The brecciated spilitic basalt of the ophiolite sequence is host to volcanogenic-related massive sulphide (VHMS or VMS) deposit of “black smoker” type of fine massive sulphides. The deposit, formed in marine environment, is associated with moderately to deeply altered basalt in brecciated zones along faults, compression fractures and probably tension fractures at depth of the syncline. The VHMS mineralization reflects a replacement type mineralization and in-fillings of pore spaces in moderately to deeply weathered basalt breccias. However, permeation type of mineralization of fine sulphide minerals occurs in volcaniclastics or remobilized volcaniclastics. Alteration in brecciated zones includes chloritization, silicification, albitization and argillization. The ophiolite, considered to be a supra-subduction zone, was emplaced in back arc setting in marginal Cotabato basin

Assay results consistently showed high Cu-Zn and elevated Au-Ag-Co credits.