1) Kunyang Rift
昆阳裂谷
1.
Kunyang rift located on the western margin of Yangtze platform is tectonically equivalent to East Africa rift where there exist modern carbonatite volcanos.
中元古代昆阳裂谷构造性质与东非裂谷相似，其中段武定海盆西缘的观天厂区段有一条ＮＥ向深大断裂通过，是碳酸质岩浆活动的有利地带。
2.
The Kunyang rift mineralization belt is one of the most significant iron and copper metallogenetic belts in Yunnan,whose deposits share a common temporal and spatial regularity,the "six stories with one ladder".
昆阳裂谷(云南段)是重要的铁铜矿化集中区,伴随裂谷的发展演化过程,铁铜矿床的成矿具有"六楼一梯"的时空分布规律,区内成矿主要受地层层位、岩相及古地理环境、构造以及火山作用等因素的控制,根据区域成矿规律特征,总结出区内4个重点找矿靶区及重要找矿地段。
2) Kunyang rift zone
昆阳裂谷带
3) Yanggu
阳谷
1.
Based on the geography culture,this article analyzed the reason of Jin Ping Mei changing the place where Takematsu killed his sister-in-law from Yanggu to Qinghe.
立足于地理文化,分析了《金瓶梅》将《水浒传》杀嫂情节的地点“由阳谷县改为清河县”的原因,进而分析了罗贯中的籍贯非东原的问题。
4) rift
[英][rɪft] [美][rɪft]
裂谷
1.
The Neoproterozoic rift systems in southern China: New evidence for the sedimentary onlap and its initial age;
华南新元古代裂谷系沉积超覆作用及其开启年龄新证据
2.
HC fluid may be generated indirectly in bottom sediments of water basins of riftogenic type under sufficiently high heat flow that do not require submersion of original oil and gas source mass at the depth of 3 km and more (riftogenic model).
指出,烃类可通过各种途径生成:烃类的生成不仅遵循传统的沉积-运移理论,而且也可生成于裂谷型底部含水沉积盆地中,当有相当高的热流时,生烃岩不需要沉降到3km以下就能生烃;在全球油气生成过程中,不能排除烃类由矿物合成的可能性;无机合成的烃类成分主要为甲烷,而生成现今的石油还需要有有机质和其他有效催化剂的加入才行,可见,石油和天然气的生成是多源的。
3.
The Liaohe Group of Paleoproterozoic Erathem located in rift basin of east Liaoning and south Jilin area ,a boron-bearing Rock series which is divided into thress part from the up to bottom of this group and separatedly locate with szaibelyite--suanite ,magnetite bearing szaibelyite and ludwigite types of boron deposits.
产于辽东-吉南地区裂谷盆地中的古元古界辽河群里尔峪组为一套含硼岩系。
5) rift valley
裂谷
1.
The spreading rate of the rift valley is estimat.
对岚皋地区辉石玢岩岩石化学和地球化学研究表明，本区辉石玢岩为碱性玄武岩系列；不同期次活动的辉石玢岩为同源岩浆在不同阶段上演化的产物；演化趋势属跨越Ｂ型，本区辉石纷岩形成于板内稳定区，是早古生代南秦岭被动大陆边缘裂谷的岩浆活动时的产物，该裂谷扩张速度与东非埃塞俄比亚相近。
2.
n this thesis, the author discussed the basic pattern of rifts in Taiwan Strait, anddivided the strait and its both sides into four rift systems, analysed the formation andevolution processes of the rift systems, explained the corresponding relation of the formation and evolution between the rift structure and rift valley, and studied the evolutionmodel of Taiwan Strait rift valley.
论述了台湾海峡新生代断裂构造基本特征，划分出海峡及两侧两大断裂系，探讨了断裂系的形成演化过程，阐明了断裂构造的形成演化与海峡裂谷演化的对应关系，并进一步探讨了海峡裂谷的演化模式。
3.
When coupled with the regional tectonic setting,it is considered that the Permian alkaline-tholeiitic basalts association in the Shuanghu Area was formed in the rift valley setting,and their occurrence may indicate a process from rift valley to juvenile oceanic crust along the Longmucuo-Shuanghu tectonic zone.
结合区域地质背景,认为双湖二叠系拉斑系列-碱性系列玄武岩组合可能形成于陆间裂谷到小洋盆环境,这套玄武岩的产出可能代表古特提斯洋沿龙木错—双湖构造带在不同地区的发育程度不同,双湖地区在二叠纪应为一个陆间裂谷到小洋盆环境。
6) Kunyang group
昆阳群
1.
Based on the stratigraphic correlation of Kunyang group(includes lithologic featutures,lithochemistry) in Tuobuka,Xiaoliukou.
通过对托布卡、小溜口、东川马鞍桥剖面昆阳群地层(包括特征岩性、岩石化学)对比研究,认为托布卡金矿矿化层位相当于东川矿区昆阳群下亚群的平顶山(美党)组和菜园湾(大龙口)组。
2.
The discovery of gold ore deposits in the Tuobuka－ Buka area is one of the very important advances made in the Kunyang Group for ore－ prospecting.
东川拖布卡-布卡地区发现的独立型金矿是滇中昆阳群找矿工作取得的重大进展之一。
3.
Carbonatic melton debris and melt inclusions have been discovered from Daqing Cubearing dolomite of Kunyang group,Middle Proterozoic Erathem in the west metallization zone of Ruoci—Wuding area Yunan province.
在云南省罗茨—武定地区西矿带中元古界昆阳群大箐亚式含铜白云岩中有碳酸盐浆屑和熔融包裹体存在。
补充资料：昆阳
【诗文】：
古木荒烟集暮鸦，高城落日隐悲笳。
并州倦客初投迹，楚泽寒梅又过花。
满眼旌旗惊世路，闭门风雪羡山家。
忘忧只有清樽在，暂为红尘拂鬓华。
【注释】：
【出处】：
古木荒烟集暮鸦，高城落日隐悲笳。
并州倦客初投迹，楚泽寒梅又过花。
满眼旌旗惊世路，闭门风雪羡山家。
忘忧只有清樽在，暂为红尘拂鬓华。
【注释】：
【出处】：
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条