鋅礦床 的英文怎麼說
中文拼音 [xīnkuàngchuáng]
鋅礦床
英文
zinc deposit-
The tianbaoshan and daliangzi pb - zn deposits, strictly controlled by " formations, phases and structures ", are typical mvt pb - zn deposits. they also belong to the epigenetic hydrothermal strata - bound deposit
天寶山、大樑子礦床嚴格受「層、相、位」的控制，屬後生熱液層控礦床，也是典型的密西西比河谷型鉛鋅礦床。The exhalation - sedimentary system of xitieshan lead - zinc deposit, qinhai province
錫鐵山鉛鋅礦床的找礦潛力與找礦方向A comparison of the prospecting model of the hf type with the prediction model of the vms type reveals that their thermal dynamic mechanisms are different : the former is related to basic - ultrabasic rock intrusion, while the latter to acidic rock intrusion
與白銀銅礦區域地球化學預測模式相比較，富鐵型鉛鋅礦床中除鐵族元素指示基性超基性巖侵入事件外，其他元素均大致相似，兩大類礦床形成的初始熱動力條件不同。Sedimentation - diagenesis deposits mainly formed during late sinian to cambrian period, such as bingtongshan pbzn deposits and aozigang deposits
沉積成巖型鉛鋅礦主要成礦時代屬晚震旦世~寒武紀，如冰洞山式鉛鋅礦床和凹子崗鋅礦床。Thermal deposits mainly formed during middle - late yanshanian age, related to extension structure, with main mineralization in qingfeng competent deformation zone, western shennongjia fault arch, northern huangling fault arch, xianfeng anticline of enshi platforman fold bundle
熱液型鉛鋅礦床主要形成燕山中晚期，與滑脫拆離構造密切相關，礦化主要集中於青峰強變形帶、神農架斷穹西部、黃陵斷穹北部、恩施褶皺束咸豐背斜、長陽褶皺束走馬坪背斜中。Genesis of lead and zinc deposit of laochang type, guangxi
廣西老廠式鉛鋅礦床成因研究Geological characterisitcs and genesis of maozu lead and zinc deposit, yunnan
鋅礦床地質特徵及成因研究Geological characters of keketale lead and zinc deposit and the discussion on its genesis
可可塔勒鉛鋅礦床地質特徵及其成因初探Geochemical anomaly model and exploration indicator of the xitieshan lead and zinc deposit
錫鐵山鉛鋅礦床地球化學異常模式及找礦指標Ore control factors of the huangshashi copper lead zinc deposit in hunan
鋅礦床控礦因素淺析Processing mineralogy of argentine in the xitieshan pb - zn deposit
錫鐵山鉛鋅礦床銀的工藝礦物學研究Discussion of geological prospecting in erlihe pb - zn deposit, fengxian
鳳縣二里河鉛鋅礦床后續地質找礦探討Distribution of anthraxolite and metallogeny of the jinding lead - zinc deposit
金頂鉛鋅礦床中碳瀝青的分佈特徵及成礦作用Fluid inclusions and metallogenic environment of the xitieshan lead - zinc deposit
錫鐵山鉛鋅礦床流體包裹體特徵及成礦環境研究Geochemical ore predicting and its effect in deep parts of xitieshan pb - zn ore deposit
錫鐵山鉛鋅礦床深部地球化學找礦預測及效果The ore - hosted strata of xitieshan lead - zinc ore deposit is located in a limb of a anticline and suffered from deformation partition
摘要錫鐵山大型鉛鋅礦床含礦巖系的構造格架位於背斜的一翼，普遍遭受變形分解作用。The model holds that the metallogenic environment of the lf type is structural reductive space whereas that of the hf type reflects entirely characteristics of sedimentary minerallization, with no evidence of tectonic minerallization
模式表明，貧鐵型礦床的成礦環境為相對封閉還原的構造空間；富鐵型礦床完整地反映了該類型鉛鋅礦床沉積成礦特點顯著，而斷裂等構造對成礦的直接影響相對不顯著。The paper discusses the deep tectonic setting of yinshan lead - zinc deposit and emphaticly studies geological features of two fault belt and relationships between deep structures and mineralization
本文論述了銀山鉛鋅礦床形成的深部構造背景，著重研究了桐柏?桐城斷裂帶、商城?麻城斷裂帶的地質特徵及其與成礦作用的關系。Geological features and prospecting potential for the shaxi ag - pb - zn deposit, batang, sichuan
四川巴塘砂西銀鉛鋅礦床特徵與找礦遠景Thus, the research on xuequan copper ( zinc ) deposit has important operation and academically significance
因此，雪泉銅（鋅）礦床的勘查研究具有重要的實際和學術意義。分享友人