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• ¡ÒÅÕ¹Ò (Galena) ÁÕÊٵ÷ҧà¤ÁÕ PbS ÁÕÊèǹ»ÃСͺ Pb 86.6% áÅÐ S 13.4% ÁÑ¡¨ÐÁÕà§Ô¹»¹ÍÂÙè´éÇ ÍÒ¨ÁÕÊѧ¡ÐÊÕ á¤´àÁÕÂÁ ¾Åǧ ÊÒÃ˹٠áÅкÔÊÁÑ·»¹ÍÂÙè´éÇ áÃè¡ÒÅÕ¹Ò ÁÕ¤ÇÒÁÇÒǤÅéÒÂâÅËÐ ¹éÓ˹ѡÁÒ¡¼Ô´»¡µÔ à¹×éÍáÃèÍè͹ ¢Ù´¢Õ´ä´é§èÒ â´ÂÍÒ¨¢Ù´´éÇÂàÅçºÁ×Í¡çà¢éÒ
• à«ÃÑÊ䫵ì (Cerrussite) ÁÕÊٵ÷ҧà¤ÁÕ PbCO₃, ÁÕ Pb 77.5 % ËÃ×Í PbO 83.5% áÅÐ CO₂ 16.5 % ÅѡɳÐÊÕ¢ÒÇ à·Ò ËÃ×ÍàËÅ×ͧ ÁÕ¹éÓ˹ѡÁÒ¡
• áͧ¡ÅÕ䫵ì (Anglesite) ÁÕÊٵ÷ҧà¤ÁÕ PbSO₄ ÁÕ Pb 68.3 % ËÃ×Í PbO 73.6% áÅÐ SO₃ 26.4 % ÊÕ¢ÒÇ à·Ò ËÃ×ÍàËÅ×ͧ

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1. Stratabound deposit of Syngenetic Origin à¡Ô´¨Ò¡¡Òà ÊÐÊÁµÑÇ µ¡¼ÅÖ¡ã¹¹éÓ·ÐàÅÃèÇÁ¡ÑºËÔ¹ªÑé¹Í×è¹æ áÅéÇà¡Ô´¡ÒÃÃÇÁµÑǡѹà»ç¹ áËÅè§áÃèã¹ÅѡɳÐà»ç¹ªÑé¹áÃèã¹ËÔ¹ªÑé¹ àªè¹ ·Õè Kupersciefer »ÃÐà·È àÂÍÃÁѹ¹Õ
2. Stratabound deposit of Epigenetic Origin à¡Ô´¨Ò¡¡Òà ÊÐÊÁµÑǢͧ µÐ¡ÑèÇ-Êѧ¡ÐÊÕ ÀÒÂËÅѧâ´ÂµÐ¡ÑèÇ-Êѧ¡ÐÊÕ ·Õè¼ÊÁÍÂÙèã¹ËÔ¹ à´ÔÁ¶Ù¡ÅÐÅÒÂÁÒÊÐÊÁµÑÇãËÁèàªè¹ ·Õè Upper Mississippi Valley ÊËÃÑ°ÍàÁÃÔ¡Ò
3. Volcano-Sedimentary deposit à¡Ô´¨Ò¡¡ÒÃÊÐÊÁµÑǢͧáÃè µÐ¡ÑèÇ-Êѧ¡ÐÊÕ¨Ò¡¡ÒûÃзآͧËÔ¹ÀÙà¢Òä¿ã¹·ÐàÅ àªè¹·Õè Kuroko »ÃÐà·È­Õè»Øè¹
4. Replacement deposit à¡Ô´¨Ò¡¡ÒÃá·¹·Õè¢Í§µÐ¡ÑèÇ-Êѧ¡ÐÊÕ ã¹ËÔ¹à´ÔÁ àªè¹·Õè Cerro dePasco »ÃÐà·Èà»ÃÙ
5. Veins à¡Ô´à»ç¹ÊÒÂáÃè àªè¹·Õè Silverton area, Colorado ÊËÃÑ°ÍàÁÃÔ¡Ò
6. Contact Pyrometasomatic deposits ¨Ò¡¢ºÇ¹¡ÒÃá»ÃÊÑÁ¼ÑÊ àªè¹·Õè Tetyukhi áÅÐ Siberia ÊËÀÒ¾â«àÇÕµ

áÃèµÐ¡ÑèÇ-Êѧ¡ÐÊÕ ã¹»ÃÐà·Èä·Â ¾ºÍÂÙè·ÑèÇä» ºÃÔàdzÀÒ¤ ¡ÅÒ§ ÀÒ¤à˹×Í áÅеÐÇѹÍÍ¡ à©Õ§à˹×Í áÅÐÀÒ¤ãµéºéÒ§ áµèÊèǹãË­èà»ç¹áËÅè§ ¢¹Ò´àÅç¡à¡Ô´à»ç¹ÊÒÂáÃè á·Ã¡¢Öé¹ÁÒã¹ËÔ¹ ã¹ÅѡɳТͧÊÒ¹éÓáÃÃé͹ (Hydrothermal Vein) ÁÕáËÅ觵СÑèÇ- Êѧ¡ÐÊÕ·ÕèÁդس¤èÒ·Ò§àÈÃÉ°¡Ô¨ ä´éá¡è áËÅ觵СÑèǨѧËÇÑ´¡Ò­¨¹ºØÃÕ ºÃÔàdzáËÅè§Êͧ·èÍ Í.·Í§¼ÒÀÙÁÔ ¨.¡Ò­¨¹ºØÃÕ ÁÕ»ÃÔÁÒ³ ÊÓÃͧ»ÃÐÁÒ³ 3,000,000 àÁµÃÔ¡µÑ¹ (µÐ¡ÑèÇ+ Êѧ¡ÐÊÕ) áÅÐáËÅè§Êѧ¡ÐÊÕ·Õè ÍÓàÀÍáÁèÊÍ´ ¨Ñ§ËÇÑ´µÒ¡ (áËÅ觼Òá´§ ÍÓàÀÍáÁèÊÍ´ ¨Ñ§ËÇÑ´µÒ¡) «Öè§ä´é·ÓàËÁ×ͧ¼ÅÔµáÃèÁÒà»ç¹ àÇÅÒ¹Ò¹áÅéÇ