保存
发表于 2025-3-28 16:23:44
http://reply.papertrans.cn/23/2288/228769/228769_41.png
破裂
发表于 2025-3-28 22:44:35
http://reply.papertrans.cn/23/2288/228769/228769_42.png
高调
发表于 2025-3-29 02:00:52
as re lated both to their intriguing form and their significance in facies inter pretation and sedimentology and to their relevance to accumulations of hydrocarbons and other mineral deposits. This resulted in numerous publications on this subject, and the intention of this volume is to sum mariz
充足
发表于 2025-3-29 07:00:36
http://reply.papertrans.cn/23/2288/228769/228769_44.png
四海为家的人
发表于 2025-3-29 10:31:54
http://reply.papertrans.cn/23/2288/228769/228769_45.png
epicardium
发表于 2025-3-29 15:10:55
Martin Mullen,Marta Giralt,Liam Murray (1977), Harris (1979), Palmer (1979) and Hine et al. (1981). The studies document facies, sedimentary structures, vertical sequences and geometry of bank-margin ooid accumulations. It is these sedimentary features that are critical in our interpretation of ancient oolite deposits seen in outcrop or borehole cores.
indoctrinate
发表于 2025-3-29 18:56:30
Activating the Brain in the Classroom,to locality, and therefore represent a small sample of compositions and fabrics possessed by coated grains. Although volumetrically insignificant, non-marine ooids from both high- and low-salinity systems are important in understanding the physical and chemical processes which give rise to variations in coated grains.
屈尊
发表于 2025-3-29 23:48:13
Classification of Coated Grains: Discussions” of Richter and Besenecker (this vol.) and some of the ooids discussed by Richter (this vol.) — thermal ooids, cave ooids, aqueduct ooids, and power plant ooids — as vadoids, though this is not justified in my opinion. This was the reason for preparing the following comment.
Mitigate
发表于 2025-3-30 00:09:01
http://reply.papertrans.cn/23/2288/228769/228769_49.png
preservative
发表于 2025-3-30 06:52:24
The Joulters Ooid Shoal, Great Bahama Bank (1977), Harris (1979), Palmer (1979) and Hine et al. (1981). The studies document facies, sedimentary structures, vertical sequences and geometry of bank-margin ooid accumulations. It is these sedimentary features that are critical in our interpretation of ancient oolite deposits seen in outcrop or borehole cores.