The Birimian Baguiomo formations are located in the northern part of the Boromo greenstone belt. In this belt, the volcanic rocks (tholeiitic basalt, calcalkaline basalt, andesite) hosting the gold mineralization are ...The Birimian Baguiomo formations are located in the northern part of the Boromo greenstone belt. In this belt, the volcanic rocks (tholeiitic basalt, calcalkaline basalt, andesite) hosting the gold mineralization are located in the Kwademen-Baguiomo shear zone. This mineralization, located only a few kilometers from the Kwademen gold deposit, is uncharacterized and, together with the latter, could constitute a gold potential capable of being economically exploitable. It is in this sense that this work is carried out with a view to characterizing the gold mineralization of the Baguiomo gold panning site. To carry out this work, we have made direct field measurements, combined with microstructures, and combined all this with data from geochemical rock analysis of the basalts that are the main host formations. Geochemical data show that tholeitic basalts formed from a mantle plume that was emplaced in an oceanic plateau context. Calc-alkaline basalts and andesites are comparable to Paleoproterozoic tholeitic basalts (PTH3), which are slightly enriched in light rare earths. Fertility tests show that these basalts concentrate between 3 and 6 ppb of gold at the time of accretion, which is sufficient for remobilization of this primary gold during the Eburnian orogeny to yield a deposit of around 4 - 5 Moz. Gold mineralization is associated with pyrite crystals when the latter are disseminated in the rock mass, whereas it is associated with hematite in quartz veins concordant with S1 shear deformation. It is mainly the pyrite crystals in the pressure shadows that contain the gold grains, whose development would be synchronous with micro-shear zone reactivation during the first phase of D1<sub>B</sub> deformation. The second phase of D2<sub>B</sub> deformation, which is a crenulation or fracture schistosity, does not significantly affect the shear deformation that controls mineralization.展开更多
目的探讨Pan-TRK免疫组化在涎腺分泌性癌(secretory carcinoma of salivary glands,SCSG)诊断及鉴别诊断中的价值。方法收集14例SCSG临床资料,采用免疫组化、FISH对SCSG进行检测。另选取经典的腺泡细胞癌、黏液表皮样癌、腺样囊性癌各1...目的探讨Pan-TRK免疫组化在涎腺分泌性癌(secretory carcinoma of salivary glands,SCSG)诊断及鉴别诊断中的价值。方法收集14例SCSG临床资料,采用免疫组化、FISH对SCSG进行检测。另选取经典的腺泡细胞癌、黏液表皮样癌、腺样囊性癌各10例作为对照。结果14例SCSG患者男女比为4∶3,年龄15~79岁,10例发生于腮腺,2例发生于颊部,1例发生于腭部,1例发生于颈部;11例生存状态良好,1例复发生存,2例失访。14例SCSG,多呈浸润性生长,呈微囊状、乳头-囊状、管状、实性排列或几者混合,腔内伴丰富分泌物,1例见神经侵犯,1例伴淋巴结转移。免疫表型:14例SCSG中CK7、S-100、Mammaglobin均阳性,11例SOX-10阳性,10例GATA-3阳性,14例DOG1均阴性,Ki-67增殖指数为1%~15%。FISH检测:12例SCSG成功检测到FISH信号,10例发现ETV6-NTRK3基因融合阳性。14例SCSG均行Pan-TRK免疫组化检测,10例细胞核阳性,1例细胞质阳性。10例腺泡细胞癌、10例黏液表皮样癌、10例腺样囊性癌中分别有2、4、7例Pan-TRK阳性,定位于细胞膜/细胞质。结论Pan-TRK免疫组化阳性可提示伴ETV6-NTRK3融合的SCSG,尤其以细胞核着色模式为阳性标准时,在SCSG诊断及鉴别诊断中表现为较高的敏感性和高度特异性,并对未来TRK基因靶向治疗提供依据。展开更多
文摘The Birimian Baguiomo formations are located in the northern part of the Boromo greenstone belt. In this belt, the volcanic rocks (tholeiitic basalt, calcalkaline basalt, andesite) hosting the gold mineralization are located in the Kwademen-Baguiomo shear zone. This mineralization, located only a few kilometers from the Kwademen gold deposit, is uncharacterized and, together with the latter, could constitute a gold potential capable of being economically exploitable. It is in this sense that this work is carried out with a view to characterizing the gold mineralization of the Baguiomo gold panning site. To carry out this work, we have made direct field measurements, combined with microstructures, and combined all this with data from geochemical rock analysis of the basalts that are the main host formations. Geochemical data show that tholeitic basalts formed from a mantle plume that was emplaced in an oceanic plateau context. Calc-alkaline basalts and andesites are comparable to Paleoproterozoic tholeitic basalts (PTH3), which are slightly enriched in light rare earths. Fertility tests show that these basalts concentrate between 3 and 6 ppb of gold at the time of accretion, which is sufficient for remobilization of this primary gold during the Eburnian orogeny to yield a deposit of around 4 - 5 Moz. Gold mineralization is associated with pyrite crystals when the latter are disseminated in the rock mass, whereas it is associated with hematite in quartz veins concordant with S1 shear deformation. It is mainly the pyrite crystals in the pressure shadows that contain the gold grains, whose development would be synchronous with micro-shear zone reactivation during the first phase of D1<sub>B</sub> deformation. The second phase of D2<sub>B</sub> deformation, which is a crenulation or fracture schistosity, does not significantly affect the shear deformation that controls mineralization.
文摘目的探讨Pan-TRK免疫组化在涎腺分泌性癌(secretory carcinoma of salivary glands,SCSG)诊断及鉴别诊断中的价值。方法收集14例SCSG临床资料,采用免疫组化、FISH对SCSG进行检测。另选取经典的腺泡细胞癌、黏液表皮样癌、腺样囊性癌各10例作为对照。结果14例SCSG患者男女比为4∶3,年龄15~79岁,10例发生于腮腺,2例发生于颊部,1例发生于腭部,1例发生于颈部;11例生存状态良好,1例复发生存,2例失访。14例SCSG,多呈浸润性生长,呈微囊状、乳头-囊状、管状、实性排列或几者混合,腔内伴丰富分泌物,1例见神经侵犯,1例伴淋巴结转移。免疫表型:14例SCSG中CK7、S-100、Mammaglobin均阳性,11例SOX-10阳性,10例GATA-3阳性,14例DOG1均阴性,Ki-67增殖指数为1%~15%。FISH检测:12例SCSG成功检测到FISH信号,10例发现ETV6-NTRK3基因融合阳性。14例SCSG均行Pan-TRK免疫组化检测,10例细胞核阳性,1例细胞质阳性。10例腺泡细胞癌、10例黏液表皮样癌、10例腺样囊性癌中分别有2、4、7例Pan-TRK阳性,定位于细胞膜/细胞质。结论Pan-TRK免疫组化阳性可提示伴ETV6-NTRK3融合的SCSG,尤其以细胞核着色模式为阳性标准时,在SCSG诊断及鉴别诊断中表现为较高的敏感性和高度特异性,并对未来TRK基因靶向治疗提供依据。
