درباره این ای-کتاب
Reservoirs generally consist of sandstones or carbonates exhibiting heterogeneities caused by a wide range of factors. Some of these formed depositionally (e.g. as channels, palaeosols, clay seams or salts), others may be diagenetic in origin (e.g. carbonate or silica cemented zones, authigenic clays, karstic surfaces). The severity with which diagenesis affects rock systems results from the interplay between the diagenetic process itself and the timescale over which it operated.
The book provides a wide-ranging overview of diagenetic processes and responses in calcareous, argillaceous, arenaceous and carbon-rich (microbial and organic) sedimentary systems. It introduces diagenetic concepts, reviews existing knowledge, and shows how existing qualitative approaches might be developed in more quantitative ways. Several chapters consider mass balance calculations and the temporal and spatial aspects of diagenetic processes. It is unique, as a textbook, in providing such a breadth of diagenetic subject range and such depth of coverage in each topic. It provides a source reference for advanced students and professionals active in reservoir and aquifer studies.
The book provides a wide-ranging overview of diagenetic processes and responses in calcareous, argillaceous, arenaceous and carbon-rich (microbial and organic) sedimentary systems. It introduces diagenetic concepts, reviews existing knowledge, and shows how existing qualitative approaches might be developed in more quantitative ways. Several chapters consider mass balance calculations and the temporal and spatial aspects of diagenetic processes. It is unique, as a textbook, in providing such a breadth of diagenetic subject range and such depth of coverage in each topic. It provides a source reference for advanced students and professionals active in reservoir and aquifer studies.
Reservoirs generally consist of sandstones or carbonates exhibiting heterogeneities caused by a wide range of factors. Some of these formed depositionally (e.g. as channels, palaeosols, clay seams or salts), others may be diagenetic in origin (e.g. carbonate or silica cemented zones, authigenic c...
کاوش موارد بیشتر
رده‌بندی این کتاب الکترونیک
نظرات خود را به ما بگویید.
اطلاعات مطالعه
تلفن هوشمند و رایانه لوحی
برنامه «کتاب‌های Google Play» را برای Android و iPad/iPhone بارگیری کنید. به‌طور خودکار با حسابتان همگام‌سازی می‌شود و به شما امکان می‌دهد هر کجا که هستید به‌صورت آنلاین یا آفلاین بخوانید.
رایانه کیفی و رایانه
با استفاده از مرورگر وب رایانه‌تان می‌توانید به کتاب‌های صوتی خریداری‌شده در Google Play گوش دهید.
eReaderها و دستگاه‌های دیگر
برای خواندن در دستگاه‌های جوهر الکترونیکی مانند کتاب‌خوان‌های الکترونیکی Kobo، باید فایل مدنظرتان را بارگیری و به دستگاه منتقل کنید. برای انتقال فایل به کتاب‌خوان‌های الکترونیکی پشتیبانی‌شده، دستورالعمل‌های مفصل مرکز راهنمایی را دنبال کنید.
