中生代中晚期的区域构造热事件是太康-济源古生界区域性高热演化形成的主控因素。
The regional tectonicthermal events in the MidLate Mesozoic were the crucial factors controlling the regional high thermal evolution of the Paleozoic in TaikangJiyuan area.
中生代晚期地温梯度高，是古生界碳酸盐岩及煤系地层的主要生气期和运移期。
The Late Mesozoic characterized by higher temperature gradient is main period of gas generation and migration of Paleozoic coal series and carbonates.
中生界海相油气勘探应集中在几个发育较好的中生代盆地，如常州、句容、无为、望江等盆地。
The oil and gas exploration in Mesozoic erathem should be focused in Mesozoic basins of fine development, for example, the basins of Changzhou, Jurong, Wuwei and Wangjiang, etc.
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