Vine Property Exploration Update

About this update from Pjx Resources Inc.

[{"type":"text","content":"Vine Property Exploration Update \n\t\t\tbody { font-size: 11pt;\n\t\t\t}\n\n\t\t\t.nr-sub-head ul,\n\t\t\t.nr-body ul {\n\t\t\t\tlist-style-type: disc !important;\n\t\t\t\tmargin-left: 2em !important;\n\t\t\t}\n\n\t\t\t.nr-sub-head ol,\n\t\t\t.nr-body ol {\n\t\t\t\tmargin-left: 2em !important;\n\t\t\t}\n\n\t\t\t.nr-body p, .nr-body {margin-bottom: 0px !important;\n\t\t\t\t\tmargin-top: 0px !important;\n\t\t\t\t\t-webkit-margin-before: 0px !important;\n\t\t\t\t\t-webkit-margin-after: 0px !important;\n\t\t\t\t\tfont-family: Arial !important;\n\t\t\t\t\tfont-size: 11pt !important;\n\t\t\t }\n\n\t\t\ttbody {\n\t\t\t\tborder-top: 0;\n\t\t\t}\n\n\t\t\t H1 {font-weight: bold;\n\t\t\t\tfont-size: 16pt;\n\t\t\t }\n\n\t\t\t H2 {font-weight: bold;\n\t\t\t\tfont-size: 12pt;\n\t\t\t }\n\n\t\t\t H3 {font-weight: bold;\n\t\t\t\tfont-size: 11pt;\n\t\t\t }\n\n\n\t\t\t H1.nr-head {\n\t\t\t \t\tfont-family: Trebuchet MS !important;\n\t\t\t \t\tfont-size: 16pt !important;\n\t\t\t \t\tcolor: #3D86C6 !important;\n\t\t\t \t\tfont-weight:bold !important;\n\t\t\t \t\ttext-align:center !important;\n\n\t\t\t }\n\n\t\t\t H2.nr-sub-head {font-weight: bold !important;\n\t\t\t \t\tdisplay: block !important;\n\t\t\t \t\ttext-align: start !important;\n\t\t\t \t\tfont-family: Arial !important;\n\t\t\t\t\tfont-size: 12pt !important;\n\t\t\t }\n\n\t\t\t .nr-body a { font-size: 11pt !important;\n\t\t\t }\n\n\t\t\t TABLE { width: auto!important;\n\t\t\t }\n\n\t\t Vine Property Exploration Update\n Toronto, Ontario (FSCwire) - PJX Resources Inc. (“PJX” or “the Company”) is pleased to announce that drilling and geophysics on the Vine Property supports the potential to discover multiple deposits in a sedimentary basin that the Company believes could be similar in size or possibly larger than the basin hosting the Sullivan deposit, located 35 kilometres north of the property.\n\n \n\nHole VA17-28 was drilled to test a VTEM airborne electromagnetic (EM) anomaly and is located approximately 2 kilometres southwest of the Eastern Gravity anomaly.  The EM anomaly appears to be associated with a massive sulphide pyrite/pyrrhotite bed, 10 cm thick, at the Sullivan time.  Disseminated sphalerite (zinc mineralization) is encountered in the 150 metres section of sediments below the Sullivan time and above the Footwall Quartzite (FWQ) se...

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