SINH KHOÁNG PERMI - TRIAS MIỀN BẮC VIỆT NAM

Permo-Triassic metalogeny of North Vietnam The Permo-Triassic period in North Vietnam has determined three ore complexes, formed in the different structures: 1/ Cu-Ni-(PGE) and Ti-Fe-V ore complex; 2/ gold-sulfide and 3/ tin-sulfide. The first complex consists of Cu-Ni-(PGE) mineralization associated with differentiated mafic-ultramafic intrusions of various volcano-plutonic types of the Song Da, Song Hien rift zones, and fold belts surrounding the Song Chay Dome. The Cu-Ni-PGE and Ti-Fe-V complexes, temporally corresponding to the two stages of plume magmatic activities: 260 Ma (Song Hien and Song Da) and 250 Ma (Phu Ngu-Lo Gam), similar to the associated ore occurrences of Emeishan LIP in Southwest of China (Limahe, Jang Baoshan, Panzhihua,...). Gold-sulfide ore complexes, including Au-As, Au-Sb, Sb-Hg-Au and Hg-Sb-(Au) types widespread in the Song Da and Song Hien rift zones as well as in Paleozoic Lo Gam and Quang Ninh folded structures. Within these structures, ore distribution in the form of ore nodes: Lang Vai, Lang Neo, Loc Shoa, Khe Chim ... Common features of these ore nodes are similar ore chemistry(Au, Sb, As, Hg) and zonation: Au-As → Au-Sb → As-Sb-Hg → Hg, as well transitional relations between different types of ore: Au-As and Au-Sb, Au-Sb and Sb-Hg (Lang Vai, Lang Neo ore nodes,...). Ages of ore formation of this complex range from 252-229 Ma, and spatial correlation with bimodal volcano - plutonic (basalt - rhyolite, rhyolite - basalt, granite - porphyry) as well as with small granite and gabbro - syenite intrusion, with age variation of about 247 -233 Ma

ĐẶC ĐIỂM HÌNH THÁI VÀ THÀNH PHẦN HÓA HỌC CỦA ZIRCON TRONG GRANITOID KHỐI NÂNG PHAN SI PAN: Ý NGHĨA CỦA CHÚNG TRONG VIỆC XÁC ĐỊNH NGUỒN GỐC ĐÁ VÀ LỰA CHỌN CHO PHÂN TÍCH ĐỒNG VỊ

Morphology and chemistry of zircon from Phanerozoic granitoids in Fansipan uplift: their significance in determination of rock type and select for isotopic analysis Based on morphological characteristics and chemical composition of zircon in the Phanerozoic granitoids in Fansipan uplift, identificable signatures of primary zircon inigneous rocks are initially established. On morphological characteristics: zircon crystals intact crystal shape with two pointed edges (tetragonal prism or pyramid crystals), is quite clear, usually colorless, yellow-brown, brown-pink color,.. Chemical characteristics of zircon: HfO2 2%, the Zr/Hf ratio in zircon from 17 to 380, these values prove the magmatic origin and correlate with the high total alkaline rocks: syenite, nepheline syenite, granosyenite,.. These characteristics have to be noted in the selection process for zircon isotopic analysis. Based on geochemical characteristics, zircon of two rock types are initially distinguished: 1/ Zircon in I-type granite (consist of granosyenite, alkaline granosyenite, quartz syenitodiorite, syenite,....), characterized by: HfO2 content 2 wt.%, the Zr/Hf ratio is high (100), the Hf/(Hf + Zr) ratio 0.025; and 2/ Zircon in A-type granite (afvedsonite bearing granite), characterized by: HfO2 content 2.5 wt.%, low Zr/Hf ratio (20), Hf/(Hf + Zr) ratio 0.025, and ThO2 and UO2 content tends to be higher than the first type

NGHIÊN CỨU TÁC DỤNG CỦA BĂNG NANO BẠC LÊN QUÁ TRÌNH ĐIỀU TRỊ VẾT THƯƠNG BỎNG

Silver was known as a strongest antimicrobial element in the nature, moreover in the nano-sized form it can modulate the wound healing process by developing pro-healing or inhibiting pro-inflammatory cytokines, resulting in accelerated wound recovery and improved cosmetic appearence. This report represents some results of using nanosilver-coated wound dressings for therapeutic treatment of burns. The dressings were manufactured by immersing non-woven fabric material into a nanosilver solution of concentration of 500 mg/l with an average size of 20 – 25 nm, which was produced by aqueous molecular solution method. The healing effect of the tested dressing was studied through the comparison with silver sulfadiazine-coated one. The experimental data obtained showed that nanosilver-coated dressing heals burns with accelerated healing and without scars, much better than silver sulfadiazine-coated dressing

ĐẶC ĐIỂM QUẶNG HÓA VÀ KHOÁNG VẬT CÁC MỎ KẼM CHÌ KHU VỰC LÀNG HÍCH

Chemical and mineralogical characteristics of Zn-Pb ores in Lang Hich areaLang Hich ore deposit consisting of 6 mining places (West Metis, East Metis, Hang Chua, Bac Lau, Mo Ba - 1Aoven, Mo Ba - 1B) was discovered in 1905 and has been exploited since 1913. Anually, the mine have been exploited ~20000 T, inspite of lacking detail investigation in mineralogy and chemistry of ores.Two mineral assemblages have been clafsified in Lang Hich deposit as followed : 1) pyrite-galenite-sphalerite (Metis,Mo Ba), 2) galenite-sphalerite (Bac Lau, Hang Chua). Basically, sphalerites, have low Fe, In contents ; Bi is medium ; Mn and Cd is high, especially, Cd have very high content. While galenite contains Ag at economical value, besides, the presence of Sb is recored. Other investigation also shows the existing of tetraedrite group, an Ag bearing mineral group, and bournonite, a Sb bearing mineral