英语翻译Indications of regional structures throughout the TCM pr

英语翻译
Indications of regional structures throughout the TCM project area are difficult to locate.In general,based on the tectonic framework of the Asam Asam Basin in the area,the main structural trend is northeast-southwest to north-south,influenced by the Meratus Range to the northwest.The boundary of the subsiding basin is marked by a number of normal faults of the same orientation.The younger sediments form a gently dipping blanket of sediments against the southern side of the Meratus Mountains and obscure many of the deep-seated structural elements resulting from the uplift of the Meratus Range.Minor folding of the younger sediments may also occur but the exact location and geometry of this folding are not clear from the data available.Some indication of folding was found between holes TCM_020,TCM_011 and TCM_017 but better recognition is required.The main faults in the area are also inferred to trend northeast-southwest to north-south.Locally,the Batu Licin Fault trends northeast-southwest and is located in the southern portion of the concession area,truncating the Tanjung Formation coal seams against the Berai Formation in the south.This implies the Batu Licin fault is a normal fault with the southern block thrown down.A regional geological map is shown on Figure 4.A structure map of seam S6 (SM),including coal thickness is shown on Figure 5.

Indications of regional structures throughout the TCM project area are difficult to locate.In general,based on the tectonic framework of the Asam Asam Basin in the area,the main structural trend is northeast-southwest to north-south,influenced by the Meratus Range to the northwest.The boundary of the subsiding basin is marked by a number of normal faults of the same orientation.
整个TCM项目范围的地域结构标识很难定位.一般来说,根据该地区的阿三阿三盆地的构造格局,主构造走向是从东北-西南到北-南方,这是受到位于西北的莫拉图斯山脉的影响所致.这沉降盆地的分界线被几个相同定向的正断层所标示.
The younger sediments form a gently dipping blanket of sediments against the southern side of the Meratus Mountains and obscure many of the deep-seated structural elements resulting from the uplift of the Meratus Range.Minor folding of the younger sediments may also occur but the exact location and geometry of this folding are not clear from the data available.Some indication of folding was found between holes TCM_020,TCM_011 and TCM_017 but better recognition is required.The main faults in the area are also inferred to trend northeast-southwest to north-south.
此年轻沉积物紧靠莫拉图斯山脉的南面形成一片平缓倾斜的覆盖沉积层,并且由于莫拉图斯山脉的隆起而掩盖了许多深层的结构元素.年轻的沉积物也可能形成小的折叠层,但是从现有的数据无法探明这折叠层的具体位置和几何结构.在TCM_020、TCM_011和TCM_017钻孔之间有折叠层的迹象,但需要更好的确认.据推测,该区域的主断层的方向也可能从东北-西南到北-南方.
Locally,the Batu Licin Fault trends northeast-southwest and is located in the southern portion of the concession area,truncating the Tanjung Formation coal seams against the Berai Formation in the south.This implies the Batu Licin fault is a normal fault with the southern block thrown down.A regional geological map is shown on Figure 4.A structure map of seam S6 (SM),including coal thickness is shown on Figure 5.
位于特许权区的南边局部的巴度里京断层伸向东北-西南方向,将紧靠着南方波赖地层的丹绒煤层截断.这意味南部区块已倾倒的巴度里京断层是正断层.图4 显示的是区域地质图.图5 标示的是S6煤层（SM）的结构图,包括煤层的厚度.
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