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云南驿
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     THE GRAVITY FLOW DEPOSITION AND ITS SIGNIFICANCE OF PROSPECTING OIL IN YUNNANYI FORMATION OF UPPER TRIASSIC,THE WESTERN MARGIN OF CHUXIONG BASIN
     楚雄盆地西缘上三叠统云南驿组的重力流沉积及其地质-找油意义
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     Research on the Lingguan Ancient-post-road Settlements of Southwest Silk Road
     西南丝绸之路灵关道(云南驿村——大田村)驿道聚落初探
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     The Carrying of Yunnan MaBang during the Republic of China
     民国时期的云南马帮驿
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     Gathering in Yunnan Province
     相聚云南
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     ZEBU CATTLE OF YUNNAN CHINA
     云南瘤牛
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     The Changes of the Post Road from Yunnan to Sichuan and Hu Guang in the Yuan Dynasty
     元代云南通四川、湖广驿路的变迁
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     On the Way of Transmigration
     再生之驿
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Taking Yongsheng and Jinguan basins and Weishan, Xiangyun, Midu, Yunnanyi basins as the structures respectively of the northern and southern ends of Changhai fault zone, it seems to show that the active segments of faults tend to show time-dependent migrations. Lateral migration is a pattern of seismicity transformation at the fault's ends. The renewed activities of the fault strengthened the seismicity. As a whole, lateral migration tends to propagate toward the earthquake belt in an adjacent area.

以永胜、金官盆地和巍山、弥渡、祥云、云南驿等盆地分别作为程海断裂北端和南端结构,不难发现,随着时间的推移,断裂的活动部位不是固定不变的。侧向迁移是端部断裂活动转化的一种形式,断裂的不断更新使程海断裂端部地震活动增强。侧向迁移总是向着区域某一条地震带方向发展。

The Upper Triassic along Xiangyun—Midu, central Yunnan is named, in ascending order, the Yunnanyi, Luojiadashan and Baitutian formstions. The lower part of Member One, Yunnanyi Fm., may be calcareous turbidite, overlying conformably the Mido Triassic Tuanshanchun Fm. The majority of upper part of the member seems to be composed of terrigenous turbidite, and the subordinate volcaniclastic turbidite can be found near Xiangyun Country. The lower part of Member Two, Yunnanyi Fm., is characterized by calcarous conglomerates,...

The Upper Triassic along Xiangyun—Midu, central Yunnan is named, in ascending order, the Yunnanyi, Luojiadashan and Baitutian formstions. The lower part of Member One, Yunnanyi Fm., may be calcareous turbidite, overlying conformably the Mido Triassic Tuanshanchun Fm. The majority of upper part of the member seems to be composed of terrigenous turbidite, and the subordinate volcaniclastic turbidite can be found near Xiangyun Country. The lower part of Member Two, Yunnanyi Fm., is characterized by calcarous conglomerates, which could be separated into two types. One is slump breccia, with the limestone gravels being from the Beiya and Zhongwo Fms. in the west (Heqing—Dali). Another maybe result from penecontemporancous gravity sliding, with the wrinkle marks indicating the paleocurrent eastwards. Sandwiched in the conglomerates is the calcareous turbidite, which becomes, ascendingly, shallow marine carbonate rocks. The member one of Luojiadashan Fm. is mainly composed of volcaniclastic sediments, with the interlayer of basaltic lava firstly discovered. The conglomerate seems to be debris flow deposits, with gravels (limestone, silicalite, granite, etc.) implying the source region in the west. In addition, the sediments of turbidity cur- rent and grain flow are well developed in the member.The sedimentary gravity flow deposits demonstrate that there might exist a rift (the central Yunnau rift) during Late Triassic, which might link the Songpan—Ganzi Trough in western Sichuann with the Youjiang rift in western Guangxi. The Triassic period might be a stage of Paleo-Tethyan relic oceanic basin, namely, the paleo-Tethys during Triassic might be composed of several relatively small oceanic basins sand some rifting troughs in southwestern China, including the central Yunnan rift. All of them might be closed and continent-continent collision occurred during the Indosinian Orogenesis, and the molasse of the Baitutian Fm. might be deposited in a hinderiand basin.

上三叠统云南驿组一段下部是钙质浊积岩,上部为陆源碎屑浊积岩及少量火山碎屑浊积岩;二段的角砾状灰岩有坍塌和重力滑动两种成因,夹钙质浊积岩。罗家大山组一段由火山碎屑质的碎屑流、浊流和颗粒流沉积组成,夹基性熔岩。它们是滇中裂谷的记录,物源区在西边,构成中国西南部三叠纪古特提斯的一部分。

The Chuxiong Basin located in central Yunnan on the southwestern margin of the Yangtze landmass is a Mesozoic peripheral foreland basin, which is bounded on the southwest by the Honghe fault, on the west by the Chenghai fault and on the east by the Puduhe fault. Tectonically, three units may be distinguished for the basin. They are: (1) western thrusting zone; (2) central depression zone, and (3) eastern uplifted zone. In terms of sedimentary facies , sequence stratigraphy and palaeogeographic evolution in...

The Chuxiong Basin located in central Yunnan on the southwestern margin of the Yangtze landmass is a Mesozoic peripheral foreland basin, which is bounded on the southwest by the Honghe fault, on the west by the Chenghai fault and on the east by the Puduhe fault. Tectonically, three units may be distinguished for the basin. They are: (1) western thrusting zone; (2) central depression zone, and (3) eastern uplifted zone. In terms of sedimentary facies , sequence stratigraphy and palaeogeographic evolution in combination with tectonic evolution of the Ailaoshan orogenic zone, the basin shows a depositional evolution from the Palaeozoic passive continental margin to the Mesozoic foreland basin. Several phases of sediments have been identified in the basin. For example, during the Carnian (Late Triassic) and the early and middle Norian (Late Triassic), the foreland flysch sediments were accentuated. while during the late Norian (Late Triassic) to the Paleocene, the foreland molasse sediments were highlighted. The molasse sediments consist of two categories: marine and continental. The latter are characterized by long time duration, widespread occurrence and greater thickness. On the whole, the basin may have experienced four stages of evolution: basin formation, rapid subsidence, inversion and filling, and final termination. The upward growth and cratonward overburden of the overthrusted orogenic wedges led to the formation of sudden deepening and fining upward sequences during the early stage and shallowing and coarsening upward sequences in the basin during the late stage. In other words, there are gradations from the early flysch sediments to the late molasse sediments, and from deep and narrow basal relief during the early stage to wide and shallow basal relief during the late stage. The centres of subsidence and deposition of the basin once in front of the thrusting orogenic wedges gradually migrated northeastwards (cratonwards). All the data on palaeocurrents, petrography, lithogeochemistry indicate multiple sources of the detritus in the basin, i.e. the detritus were derived dominantly from the ancient Ailaoshan orogenic zone, and subordinately from the eastern uplifted zone.

楚雄盆地位于扬子陆块的西南边缘,为一中生代周缘型前陆盆地。根据沉积相特征、层序地层结构和古地理演化的详细研究,结合古哀牢山造山带的构造演化,笔者认为楚雄盆地经历了从古生代被动大陆边缘沉积到中生代前陆盆地沉积的演化。前陆盆地演化的阶段性明显:晚三叠世卡尼期(云南驿组沉积期)和诺利早、中期(罗家大山组沉积期)为前陆复理石沉积;诺利晚期(花果山组沉积期)—古新世(赵家店组沉积期)为前陆磨拉石沉积。磨拉石沉积可分为海相含煤磨拉石和陆相红色磨拉石两种类型。其中陆相磨拉石沉积时间跨度长,分布面积广,沉积厚度大,沉积演化可细分为盆地成形、强烈沉降、回返充填和萎缩消亡四个阶段。随着逆冲造山楔的不断向上生长和向克拉通方向加载,楚雄前陆盆地经历了一个早期向上突然加深、变细和晚期向上变浅、变粗的沉积充填过程;盆地由早期复理石沉积演变为晚期磨拉石沉积;盆地基底形态由早期的窄而深演化为晚期的宽而浅;分布于造山楔前缘的盆地沉降与沉积中心也不断地向北东克拉通方向迁移。古流向、岩石学和岩石地球化学数据都显示楚雄前陆盆地沉积物的主要物源区为古哀牢山造山带,其次为东部隆起带,因此,盆地沉积物的供给具有明显的双物源特征。

 
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