Pore fluid chlorinity lower than seawater is often observed in accretionary wedges and one of the possible causes of pore water freshening is the smectite to illite reaction. This reaction occurs duri

DataONE2017-08-05 更新110

Interstitial water chemistry of Hole 2-8A

孔隙水地球化学

沉积物成岩作用

Details given in volume 2, chapter 15

B2FIND60

(Appendix A) Rock magnetic results with indication of the diagenetic setting of ODP Site 204-1251

岩石磁学

沉积物成岩作用

Sulphate zone <3 mbsf, sulphate-methane transition 3-6 mbsf, bottom simulating reflector 193 mbsf

PANGAEA00

(Appendix A) Rock magnetic results with indication of the diagenetic setting ...

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(Appendix A) Rock magnetic results with indication of the diagenetic setting ...

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