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Three-dimensional kinematic history at an oblique ramp, Leamington zone, Sevier belt, Utah

机译:犹他州塞维尔地带Leamington区斜坡的三维运动史

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Differences in kinematics in adjoining salients in fold-thrust belts are typically accommodated along bounding transverse zones. The Leamington zone is an oblique ramp that accommodates slip between structures in the Provo salient and the central Utah segment of the Sevier fold-thrust belt. The Leamington zone consists of the Leamington Canyon thrust, associated second-order asymmetric folds and an out-of-syncline reverse fault. The Leamington Canyon thrust is a rotated, SE-dipping thrust fault with top-to-southeast motion; it represents an oblique ramp of the folded Canyon Range thrust. Fold tightening of the syncline SE of the folded Leamington Canyon thrust trace during later emplacement of underlying structures, caused out-of-syncline reverse faulting in the fold-core. Analysis of the finite strain, minor fault populations, and conjugate fracture sets were used in interpreting the 3-D kinematic history along the Leamington zone. Restored maximum stretching directions of finite strain ellipsoids trend eastward overall. Inferred motion planes from populations of slickenlines on minor faults are consistent with overall southeastward motion. Acute bisectors of conjugate fracture sets may reflect more southward directions later in the deformation history. These superimposed deformations, with local relative chronologies of plastic and brittle structures using cross-cutting relationships, indicate that the Leamington zone area shows overall clockwise changes in kinematic directions from E to ESE to SSE during successive pulses of deformation. The temporal changes in kinematic directions along the Leamington zone most likely reflect variations in kinematics over the oblique ramp as the overall easterly displaced 3-D fold-thrust belt wedge interacted with the pre-existing oblique ramp structure, with small magnitudes of superimposed local vertical-axis rotations during later folding and fold-tightening of the Leamington Canyon thrust.
机译:通常沿边界横向区域适应褶皱-冲断带中相邻凸体的运动学差异。皇家利明顿带是一个倾斜坡道,可以容纳普罗沃凸面构造与塞维尔褶皱冲断带犹他州中段之间的滑动。利明顿带包括利明顿峡谷逆冲断层,相关的二阶不对称褶皱和不同步斜向逆断层。皇家利明顿峡谷逆冲是旋转的,东南倾角的冲断断层,由顶向东南运动。它代表折叠后的Canyon Range推力的倾斜坡道。折叠的Leamington Canyon推力迹线的向斜线SE的折叠收紧在下层结构的后续放置期间引起了折叠线芯的向斜线反向断裂。对有限应变,次要断层总体和共轭断裂组的分析用于解释沿Leamington带的3-D运动史。恢复的有限应变椭球体的最大拉伸方向总体上向东。从少量断裂上的滑线群推断出的运动平面与总体东南运动一致。共轭裂缝组的急性平分线在变形历史的后期可能会向南反射更多。这些叠加的变形以及使用横切关系的塑性和脆性结构的局部相对时间关系,表明在连续的变形脉冲期间,Leamington带区域显示出从E到ESE到SSE的运动方向上的整体顺时针方向变化。沿Leamington区运动学方向的时间变化很可能反映了斜坡道上的运动学变化,因为整体东移的3-D褶皱冲断带楔与原有斜坡道结构相互作用,且局部叠加的垂直幅度较小勒明顿峡谷推力的后续折叠和折叠拧紧过程中的轴旋转。

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