摘要：在岩浆侵入体热作用下，塔里木盆地下古生界碳酸盐岩局部发生了大理岩化作用。
Abstract: the Lower Paleozoic carbonates of Tarim Basin were marbleized locally due to the thermal effects of magma intrusions.
在岩浆侵入体热作用下，塔里木盆地下古生界碳酸盐岩局部发生了大理岩化作用。
The Lower Paleozoic carbonates of Tarim Basin were marbleized locally due to the thermal effects of magma intrusions.
塔里木盆地西北缘巴楚县的塘王城剖面是大理岩化作用较为典型的野外剖面，塔中地区的中16井是揭示大理岩化作用较为典型的钻井。
Marmorization is typical on the Tangwangcheng outcrop section in Bachu county at the northwestern margin of Tarim Basin and in cores from Well Zhong-16 in the Tazhong area.
塔里木盆地西北缘巴楚县的塘王城剖面是大理岩化作用较为典型的野外剖面，塔中地区的中16井是揭示大理岩化作用较为典型的钻井。
Marmorization is typical on the Tangwangcheng outcrop section in Bachu county at the northwestern margin of Tarim Basin and in cores from Well Zhong-16 in the Tazhong area.
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