Carbonate-clastic transitions
by Doyle, Larry J., Roberts, Harry Heil
fromDevelopments in sedimentology
by Doyle, Larry J., Roberts, Harry Heil
fromDevelopments in sedimentology
by Doyle, Larry J., Roberts, Harry H.
fromDevelopments in sedimentology
Over the years, the field of sedimentology has become subdivided into various specialities. Two of the largest groups are those who study clastic rocks and those who study carbonates. There is little communication between the two: journals appear which are exclusively devoted to…
by Doyle, Larry J., Roberts, Harry H.
fromDevelopments in sedimentology
During the past decade, work on cool water carbonates has expanded to become a mainstream research area. Studies on modern and Quaternary deposits will continue to be important; however, there is increasing momentum towards unravelling sediment processes, biota-sediment interact…
During the past decade, work on cool water carbonates has expanded to become a mainstream research area. Studies on modern and Quaternary deposits will continue to be important; however, there is increasing momentum towards unravelling sediment processes, biota-sediment interact…
Carbon trapped in diamonds and carbonate-bearing rocks in subduction zones are examples of the continuing exchange of substantial carbon between Earth's surface and its interior. However, there is still much to learn about the forms, transformations, and movements of carbon deep…
Carbonate mineral formation in lakes is a consequence of the interactions of lake water chemistry, physical processes at several scales, and biological influences, all of which are greatly affected by individual lake basin attributes such as basin size and physiography, bedrock …