CAJ | 학술논문

垦丁混杂岩出露于台湾南部恒春半岛中新世增生楔内,长约20 km,宽最大可达1 km,呈北西-南东向狭长带状分布,大致平行于马尼拉海沟北段,其分布特征类似于与俯冲板块边界相关混杂岩的特征,因此垦丁混杂岩成因的确定对于了解台湾造山带结构及构造演化历史具有重要意义。关于垦丁混杂岩成因,目前主要分为沉积(olistostrome)成因和构造成因两大观点。通过野外观察,垦丁混杂岩的泥质基质普遍发生强烈的剪裂作用,鳞片状结构大量发育,基性或超基性的外来岩块夹杂其中。此外,在垦丁混杂岩内还发现香肠化的砂岩块、由泥质基质充填的脉体及砂岩表面的水压破裂等构造现象。这些现象均反映垦丁混杂岩为构造成因而非沉积成因。垦丁混杂岩体原形成于增生楔底部,并受到一定的高压及应力剪切作用,之后随同卷入的外来岩块及连续沉积地层块体一起沿着马尾逆断层出露于地表浅部,代表南海洋壳向东俯冲于菲律宾海板块之下形成的构造混杂堆积岩体。
은정혼잡암출로우태만남부항춘반도중신세증생설내,장약20 km,관최대가체1 km,정북서-남동향협장대상분포,대치평행우마니랍해구북단,기분포특정유사우여부충판괴변계상관혼잡암적특정,인차은정혼잡암성인적학정대우료해태만조산대결구급구조연화역사구유중요의의。관우은정혼잡암성인,목전주요분위침적(olistostrome)성인화구조성인량대관점。통과야외관찰,은정혼잡암적니질기질보편발생강렬적전렬작용,린편상결구대량발육,기성혹초기성적외래암괴협잡기중。차외,재은정혼잡암내환발현향장화적사암괴、유니질기질충전적맥체급사암표면적수압파렬등구조현상。저사현상균반영은정혼잡암위구조성인이비침적성인。은정혼잡암체원형성우증생설저부,병수도일정적고압급응력전절작용,지후수동권입적외래암괴급련속침적지층괴체일기연착마미역단층출로우지표천부,대표남해양각향동부충우비률빈해판괴지하형성적구조혼잡퇴적암체。
The Kenting Mélange located in the Central Range-Hengchun Peninsula accretionary prism shows a chaotic block-in-matrix structure. It was considered to be mainly of sedimentary origin (olistostromes) in the early 1990s, but tectonic origin gradually becomes a mainstream point of view when a large number of marine data has been collected since 1990s. According to lots of field observation, we find these chaotic deposits consist of a variety of blocks, up to km in size, of different lithologies such as chrome-spinel, gabbros, basalt and sandstones. These blocks float in a muddy matrix commonly showing a pervasive scaly foliation. Moreover, sausage-shaped sandstone, mud veins intruded in the exotic blocks under high pressure and heterogeneous hydrofracture in the surface of sandstones can demonstrate the Kenting Mélange was a tectonic origin rather than olistostromes. The Kenting Mélange can be considered as a mega-sheared fault zone about 1 km wide and 20 km long that approximately parallel to the north part of Manila trench, it is the character of tectonic mélange as fault rock of subduction plate boundary. In comparing the Kenting Mélange with the famous tectonic mélange in the world such as the Mugi Mélange in the Shimento Belt, Japan and the Bobonaro Mélange in the western Banda orogen, Indonesia, it is interesting to note the similarities. Moreover, seismic reflection profiles and foraminifera analysis studied before can also support the tectonic origin. In summary, a hypothesis can be proposed that the Kenting Mélange is a tectonic mélange as fault rock of subduction plate boundary at the front of the Taiwan accretionary prism, it formed mostly at the base of the accretionary prism by stratal detachment and fluid-assisted remobilization above a basal decollement, and then exposed through the splay fault system along with the involvement of the exotic blocks and the original continuous sedimentary strata block. The Kenting Mélange represents fault rock of subduction plate boundary during the subduction of South China Sea beneath the Philippine Sea Plate, which is located near the boundary of Philippine and Asian plates.