1) Cambrian source rock
寒武系烃源岩
1.
It is not sure whether the Cambrian source rocks or the Middle and Upper Ordovician ones or both of them made contributions to the organic matters in the Silurian asphaltic sandstones.
塔里木盆地志留系沥青砂岩广泛发育,主要原因是来源于寒武系的原油在进入志留系储层后区域性的抬升剥蚀使油藏遭到严重破坏,但到目前为止,究竟是寒武系烃源岩还是中上奥陶统烃源岩或是两者都对现今的志留系沥青砂岩中的有机质有贡献还不清楚。
2) Cambrian period limestone
寒武系灰岩
1.
Cambrian period limestone has the characteristic of strong aquosity, high water-pressure and sudden inflow of water in Laangbei coal mine.
寒武系灰岩富水性强,水压高,初采工作面均发生突水,梁北煤矿认真总结经验教训, 科学运用向寒武系灰岩加固煤层底板的新技术,实现了工作面安全回采。
3) source rock measures
烃源岩系
1.
Based on sedimentological and geochemical theories, this paper have studied and discussed more profoundly about the source rock measures of Jianchang-Kazuo basin.
本文根据沉积学和地球化学原理,对建昌—喀左盆地烃源岩系进行了比较深入的研究。
4) Cambrian carbonate rock
寒武系碳酸盐岩
1.
The ore bodies which occurrences are in conformity to wall rock's and are stratiform-like or stratiform occur in Cambrian carbonate rock(including Qingxudong formation, Gaotai formation,Pingjing formation, Gengjiadian formation), and they are roughly controlled by the infiltration of wall rock and formed during .
产状与围岩基本与一致的层状、似层状矿体产于寒武系碳酸盐岩中(以清溪洞组、高台组、平井组、耿家店组为主)，这些矿体主要受主岩渗透性控制，为加里东期的产物，但寒武系中部分脉状、透镜状的富矿体为燕山期的产物。
6) Precambrian succession
前寒武纪岩系
补充资料：烃源岩(见生石油天然气岩层)
烃源岩(见生石油天然气岩层)
source rock of oil and gas
、~u以人‘峪iUU长天然气岩层01012丹nd即劝见生2
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条