the sequence develops a three-divided system tracts 層序發(fā)育三分體系域。
paleogene lowstand system tract deposits and nonstructural traps in dongying sag 東營(yíng)凹陷下第三系低位域沉積及非構(gòu)造圈閉
transgressive system tracts and related reservoir bodies of paleogene in western qaidam basin 柴達(dá)木盆地西部古近系湖侵體系域及相關(guān)儲(chǔ)集體
yaojia formation and the member-one nenjiang group are lake expanding system tract of sequence 2 姚家組和嫩江組一段是層序2的湖泊擴(kuò)張?bào)w系域。
for a long time, the above division of systems tracts has been a classical model in the study of continental deposition 長(zhǎng)期以來,從國(guó)外傳入的三個(gè)水位域沉積體系劃分成為研究陸相沉積的經(jīng)典模式。