The palaeostructure high part of Carboniferous in Indosinian epoch is favourable to the development of burial corrasion pores.
石炭系印支期的古构造高部位是埋藏溶解孔发育的有利地区。
The palaeostructure high part of Carboniferous in Indosinian epoch is favourable to the development of burial corrasion pores.
石炭系印支期的古构造高部位是埋藏溶解孔发育的有利地区。
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