left-oblique 中文意思是什麼
left-oblique
解釋
左傾斜的-
According to the spread of nappe and relation between the nappe and depression, oblique - thrust fault zone was divided into three parts in this paper : sertengshan, lvliangshan and xitieshan. ( 3 ) according to macroscopic characteristics of fault zone, cleavage characters of fault zone, drag folds, the reverse " s " fold in the footwall, positive flower structures and small left strike - slip fault, the kinematics characters of fault zone of sertengshan - xitieshan are concluded : thrusting in section, left - slip fault in plane and the strike - slip displacement increasing from the west to the east
（ 3 ）根據斷裂斷裂帶的宏觀特徵、斷層帶劈理特徵、斷裂帶附近的牽引褶皺和斷層下盤的平面反「 s 」型褶皺以及斷層上盤剖面正花狀構造和平面左行小型平移斷層，認為賽什騰-錫鐵山斷裂帶運動學主要表現為剖面上的逆沖、平面上的左行走滑特點，並且走滑量具有自西向東增大之勢。 -
There are coherent between the spread of oblique - thrusting structure, fold and fault structure. there were close relationships between oblique - thrust structure and the reverse " s " structure in the basin. both of them are result of the left oblique - thrusting
逆沖推覆構造呈斜列式形展布與盆地內的也呈斜列式反「 s 」形展布的構造具有密切關系，都屬于斷裂左行斜沖的產物。 -
Computerized tomography showed inferior rectus muscle enlargement in the right eye and inferior rectus, medial rectus, and superior oblique muscle enlargement in the left eye
經電腦斷層顯示，右眼下直肌和左眼下直肌、內直肌以及上斜肌有肥厚的現象。 -
Left - anterior oblique view
左前斜位 -
Left hand ap oblique
右手正斜位 -
Eye movement revealed limitation of superior rectus, lateral rectus, and inferior oblique muscles of left eye
眼球運動顯示左眼上直肌，外直肌，及下斜肌功能受損。 -
Thrusting is the main character, so it was named as left - slip oblique - thrusting fault
但總體以逆沖為主。因此，將其稱為左行斜沖斷裂構造。 -
( 5 ) according to the study on seismicic data, sedimentary characteristics, contact relations, incision relation of the faults and strata related to the folds which are associated with the faults, this paper reached the conclusions : the oblique - thrusting structure of sertengshan - xitieshan in northern qaidam basin was formed in middle jurassic and the left - thrusting fault zone was established in the late pliocene of neogene
（ 5 ）根據地震質料、沉積特徵、地層的沉積接觸關系、斷裂切割地層關系以及與斷裂相關的褶皺捲入地層的研究，認為柴達木盆地北緣的賽什騰? ?錫鐵山逆沖推覆構造形成於中侏羅世，而左行逆沖斷裂帶定型于新第三紀上新世末。
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