Sedimentary and structural history of the Texel-IJsselmeer High, the Netherlands
Sedimentary and structural history of the Texel-IJsselmeer High, the Netherlands
复制标题
荷兰特塞尔-艾瑟尔湖高地的沉积和构造历史
DOI：
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发表时间：
1996
期刊：
影响因子：
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通讯作者：
M. Geluk
中科院分区：
文献类型：
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作者：
R. Rijkers;M. Geluk
Texel-IJsselmeer高地位于荷兰北部，是一个北西-东南走向的断块，略微向东北倾斜。它影响了晚石炭世-早二叠世至第三纪地区的沉积模式和构造发育。高压影响了晚侏罗世和早白垩世二叠纪（上Rotliegend和zechstein）相的分布和沉积过程。晚侏罗世高位的隆升和同时期邻近盆地的沉降与地壳伸展有关。坳陷南缘晚侏罗世断裂伴上盘沉降（荷兰中部盆地）和下盘隆升（Texel-IJsselmeer高地和Friesland地台）。这导致了对高地的严重侵蚀，这可以用地壳的等等温模型来模拟。在晚白垩世-早第三纪反转阶段，沿原侏罗系断裂在高压正南侧发生逆断裂。在高产气的二叠系砂岩和碳酸盐岩两侧发现了良好的储层特征。在当地，下白垩统砂岩在Friesland平台上产气。
The Texel-IJsselmeer High, in the northern part of the Netherlands, is a NW — SE trending fault block, slightly tilted to the northeast. It affected sedimentation patterns and the structural development of the area from the Late Carboniferous — Early Permian to the Tertiary. The high influenced both the Permian (Upper Rotliegend andZechstein) facies distribution and the sedimentary processes during the Late Jurassic and the Early Cretaceous.Uplift of the high during the Late Jurassic and contemporaneous subsidence of adjacent basins can be linked with crustal extension. Late Jurassic faulting at the southern edge of the high was accompanied by hanging-wall subsidence (Central Netherlands Basin) and footwall uplift (Texel-IJsselmeer High and Friesland Platform). This resulted in significant erosion on the high, which can be modeled with an isocratic model of the crust. During the Late Cretaceous — Early Tertiary inversion phase, reverse faulting occurred along pre-existing Jurassic faults in a zone directly to the south of the high. On both sides of the high, gas-producing Permian sandstones and carbonates have been found with good reservoir characteristics. Locally, Lower Cretaceous sandstones are gas-producing on the Friesland Platform.