Vertically , a series of turbidite fans and fan deltas developed along eastern border of guxi contemporaneous fault zone and sandbodies were overlaped with each other 垂向上，沿东部边界孤西同生断裂带发育的一系列浊积扇和扇三角洲由于迁移摆动，砂体可以相互叠置连片。
I remember that you said death is psychologically just as important as birth , and likely is an integral part of life , but surely it can ' t be like birth , it is an end , can ' t 我记得您说过，死同生一样重要，就像生命的一个完整的部分，但它确实不能同生相提并论，死亡是个结束，不是吗？
Can those living in the present soberly and humbly put away their prejudices as they look back , and learn lessons from the past , so as to create a better future for generations to come 有缘同生在当世的人，是不是可以在共同回首之际，冷静而虚心的放下成见，吸取教训，为子孙创造更美好的将来？
Can those living in the present soberly and humbly put away their prejudices as they look back in retrospection , and learn lessons from the past , so as to create a better future for generations to come 有缘同生在当世的人,是不是可以在共同回首之际,冷静而虚心的放下成见,吸取教训,为子孙创造更美好的将来？
Can those living in the present soberly and humbly put away their prejudices as they look back in retrospection , and learn lessons from the past , so as to create a better future for generations to come 有缘同生在当世的人，是不是可以在共同回首之际，冷静而虚心的放下成见，吸取教训，为子孙创造更美好的将来？
Activities of the fault zone led to the change of sedimentary facies , and a large number of grativity sedimentation and grativity sliding structures were developed along the slope contolled by the fault zone , with volcanic activities 同生断裂活动导致了沉积相的显著变化，沿断裂形成的斜坡上发育有大量的重力流沉积和重力滑动构造，并伴有火山活动。
From the characteristic of district gravity , the characteristic of remote sension . we can see that ore area develops south - north consotium rift . it not only controls the eastern edge of zhenxun basin , but also controls the form of bed 矿床类型以沉积、沉积?改造型为主。根据区域重力特征、卫星影象和其他地质特征，矿区所在部位，发育南北向的同生断裂。
The immediate host siliceous rocks of typical deposits ( jinya , gaolong ) are of hydrothermal sedimentary origin . gold ore bodies are layer - like and generally concordant with their host rocks . abundant relict synsedimentary fabrics are preserved in the ores 典型矿床(金牙、高龙)中的含矿硅质岩属热水沉积岩，矿体形态主要为与地层整合的层状和似层状，矿石具有大量同生沉积的标型组构。
Two kinds of ore have been identified . the first type is characterized by syngenetic sedimentation , which is called as hot - water sedimentary ore . the ore emerges in bedded orebodies which have stable thickness 作为典型矿例的佛子冲矿田主要产于下志留统细碎屑岩夹碳酸盐岩地层中，作者首次在矿田内发现了两种不同矿石类型：一类矿石具有典型的同生沉积特征，称之为热水沉积型矿石，矿石产于层状、似层状矿体中。
There are a series of lead - zinc polymetallic deposits , such as fozichong , dongtao , xiashui , wenlongjing and jilongding distributed along the fault zone . these deposits have some similiar features : ? ll of them are bounded in the strata of lower palaeozoic group ; ? ain orebodies occur as stratiform or stratoid form with occurrence consistent with that of host strata ; ? tratiform skam or baritic rock are the direct country rock of orebodies ; ? ypical syngenetic sedimentary fabric preserved in the ore . these deposits may be included in the same metallogenic series 佛子冲、东桃、下水、文龙径、鸡笼顶等一系列铅锌多金属矿床沿该断裂带分布，这些矿床虽然在成矿规模、赋矿层位和矿石矿物组成等方面存在一些差异，但均产于下古生界地层中；主要矿体呈层状、似层状产出，与地层产状大体一致；直接赋矿围岩为层状绿色岩或重晶石岩；矿石中保留有典型的同生沉积组构。
