markit meaning in English
麦盖提
Examples
- However , the true reason that markit slope are so steep is due to intense tectonic movement of late himalayan . as concerned as this hydrocarbon source regional evolution , the key tectonic movements for hydrocarbon accumulation can be divided into three stage : ( 1 ) middle - late caledonian movement ; ( 2 ) late - terminal hercynian movement ( 3 ) late himalayan movement
给合本区的烃源岩演化史，对本区油气运聚成藏关键性的构造运动有三期：中晚奥陶的伽里东中晚期运动；早晚二叠的海西晚、末期运动喜马拉雅晚期。 - By digussing the key exploration area of each structural unit , this paper pointed out : ( 1 ) look for the paleo - reservior foemed in late hercynian and second reservoir formed in himalyan periods in the west part of bachu arch ; ( 2 ) key exploration area in the east of bachu arch is middle - low cambrian self - generation and self - reservoir inside primary reservior . ( 3 ) the exploration on markit slope should focus on paleohigh formed during late caledonian , residual paleo - reservior ( middle - low cambrian primary inside reservoir , ordovician weathering crust oil / gas pool ) and subtle oil / gas trap formed in late period
分析讨论了每个构造单元的勘探重点：在巴楚隆起西段应以寻找加里东期和海西晚期形成古油藏和喜山期形成的次生油藏为重点；巴楚隆起东段应以中下寒武的自生自储的原生内幕油气藏为主要勘探目标；麦盖提斜坡应以伽里东中晚期形成的古隆起，海西晚期形成的，现未被完全破坏的残留古油藏(中下寒武原生内幕油气藏、奥陶系风化壳油藏)和以石炭二叠为烃源岩的晚期成藏的隐闭油气藏二者并重的方针。 - In order to furtherly study the petroleum accumulation law , this paper , based on the tectonic evolution , started from main hydrocarbon generation periods of the main resource rock , analysed petroleum generation , migration , accumulation , adjustment and dynamic accumulation process . according to area structural characteristic , bachu - markit was divided into the three sub - structure unit , that is , east part of bachu arch , west part of bachu arch and markit slope and established accumulation model of each part
为了更深入的分析油气聚集规律，本论文从主力烃源岩的主生油期出发，避开细枝末节，以区域构造演化为线索，分析油气生成，运移，聚集，破坏调整，再次运聚成藏的动态过程。根据巴楚?麦盖提地区的区域构造特点，将该区分为三个次级构造单元，即巴楚隆起西段、巴楚隆起东段、麦盖提斜坡，分别建立了成藏模式。 - Bachu arch is a common forland uplift of southwest of tarim forland basin northeast of tarim forland basin . this arch previously is a low submerged paleohigh which rised integrality above water from late hercynian to terminal hercynian , was exposed to denudation mostly because of uplifting integrality in mesozoic , ulteriorly uplifted and strongly reformed in late himalayan . markit slope is a slope north dipping in early paleozoic , tilted in south - north orientation in hercynian
巴楚隆起作为塔西南前陆盆地和塔东北前陆盆地的共用前陆隆起，是一个早古生代潜伏于水下的低隆，海西晚期至末期呈整体性隆升，露出水面，中生代整体隆升，大面积遭受剥蚀；喜马拉雅晚期进一步隆升和强烈被改造，才定型成现今的构造格局。 - Bachu arch is a large back - thrust uplift . tectonic evolution of its large boundary fault fracture have relation with oil / gas distribution involuntarily . its large boundary fault fracture is basement rift formed in late hercynian period and strongly actived in late himalayan period . oil / gas distribution of bachu - markit have relation with fault interspace distribution . so , this paper also discussed interspace distribution and movement stage of fault
巴楚隆起是一个大型背冲断隆，其边界大断裂的形成演化自然关系到本区的油气分布，隆起的边界大断裂多是海西晚期形成的基底断裂，后在喜山期强烈活动，兼具压扭走滑性质。