泥巖
This study focuses on the understating of morphological characteristics and evolutionary model in the mud rock area, southern Taiwan. 摘要:二仁溪流經(jīng)臺灣西南部泥巖分布區(qū)，呈現(xiàn)惡地地形及曲流地形。
After the construction,a binded rock mass with the grouted vein as its skeleton was formed from the collapsed mud rock flow like loopse l... 施工后，原塌落的泥石流狀態(tài)的松散層形成了以注漿脈為骨架的結(jié)石體，在完全沒有支護的情況下，巷道能自穩(wěn)，對類似礦山具有推廣價值。
Based on the collected data of mud rock flow in combination with rainfall condition, the author puts forward the early warning precipitation and range for slope mud rock flow, slide mud rock flow and gully mud rock flow and countermeasures. 根據(jù)大苗山已經(jīng)收集到的泥石流資料，結(jié)合降雨情況，提出坡面泥石流、滑坡泥石流和溝谷泥石流預(yù)警雨量和預(yù)警范圍、治理措施。
It is proved that the Bottom Aquifer was composed of diluvial alluvial deposition and beds bearing gravel were mainly formed by rapid mud rock flow in fault basins during Miocene epoch when the paleoclimate was warm and dry. 各礦區(qū)的底含皆形成于氣候干暖的新第三紀(jì)中新世 ,是一套在中、新生代斷陷盆地內(nèi)的山前洪積扇上由快速水流形成的洪積 -沖積物 ,含礫石地層多為泥石流沉積物
The moment high pressure of magma intrusion caused brittle fracture of the surroundings mud rocks,and tension and compression fissures . 巖漿侵入活動大大改變了其周圍泥巖的儲集性能,對油氣聚集具有重要意義。
On Mud Rock Flow in Damiao Mountain 大苗山泥石流研討
