@article{coleman1897clastic,
    author = "Coleman, A. P.",
    title = "Clastic Huronian rocks of western Ontario",
    year = "1897",
    journal = "Geological Society of America Bulletin",
    url = "https://doi.org/10.1130/gsab-9-223",
    doi = "10.1130/gsab-9-223",
    number = "1",
    openalex = "W2324747455",
    pages = "223-238",
    volume = "9"
}

@article{blackwelder1917characteristics,
    author = "BLACKWELDER, E.",
    title = "Characteristics of continental clastics and chemical deposits",
    year = "1917",
    journal = "Geological Society of America Bulletin",
    url = "https://doi.org/10.1130/gsab-28-917",
    doi = "10.1130/gsab-28-917",
    number = "1",
    openalex = "W2315763803",
    pages = "917-924",
    volume = "28"
}

@article{doi101086624388,
    author = "Fraser, H. J.",
    title = "Experimental Study of the Porosity and Permeability of Clastic Sediments",
    year = "1935",
    journal = "The Journal of Geology",
    abstract = "The purpose of this study is threefold: to experimentally evaluate the factors controlling the porosity and permeability of ideal clastic materials; to determine the modifications produced in natural deposits by variations from the ideal; to apply the principles of permeability to the problem of the distribution and localization of mineral deposits in clastic sediments. The effect on porosity of absolute grain-size, variable grain-size, shape of grain, method of deposition, and compaction are experimentally determined for ideal materials and compared with those of river and beach sands and other clastic sediments. Various equations for permeability are discussed; and the controlling factors of temperature, hydraulic gradient, size and shape of grain, uniformity of grain-size, porosity, and stratification are experimentally evaluated for ideal materials, and the modifications caused by natural materials are delimited and discussed. Field observations on the effects of wave and river depositional processes on porosity and permeability are presented. Comparisons are made of the relative permeability of gravel, sand, clay, loess, till, and unsorted alluvium. Changes produced in the original porosity and permeability of clastic sediments by the metamorphic processes of compaction, cementation, and recrystallization are outlined. Finally, the principles governing the flow of fluids through unconsolidated clastic materials are applied to the flow of hydrothermal solutions through rocks of clastic origin in an attempt to use the principles of permeability to explain and predict the distribution and localization therein of hydrothermal mineral deposits.",
    url = "https://doi.org/10.1086/624388",
    doi = "10.1086/624388",
    openalex = "W1985365761"
}

@misc{goldberg1976conditions1,
    author = "Gol'dberg, I. S. and Zelichenko, I. A. and Chernikov, K. A",
    title = "Conditions for the appearance of the main phase of oil formation in clastic rocks of the Mesozoic and Paleozoic [in Russian]",
    year = "1976",
    howpublished = "Geologiya Nefti i Gaza, v. 3, p. 57- 63; English summary in Petroleum Geology, v.14, no.3, 1977, p.135-137",
    note = "talkorigins\_source = {true}; raw\_reference = {Gol'dberg, I. S., Zelichenko, I. A., and Chernikov, K. A., 1976, Conditions for the appearance of the main phase of oil formation in clastic rocks of the Mesozoic and Paleozoic [in Russian]: Geologiya Nefti i Gaza, v. 3, p. 57- 63; English summary in Petroleum Geology, v.14, no.3, 1977, p.135-137.}"
}

@misc{samsonov1977epigenetic3,
    author = "Samsonov, V. V. et al",
    title = "Epigenetic cementation of terrigenous collectors and special features of bitumonites spreading on the southern slope of the Nepskii arch",
    year = "1977",
    howpublished = "Geology of Oil and Gas, v. 2, p. 18-25",
    note = "talkorigins\_source = {true}; raw\_reference = {Samsonov, V. V. et al., 1977, Epigenetic cementation of terrigenous collectors and special features of bitumonites spreading on the southern slope of the Nepskii arch: Geology of Oil and Gas, v. 2, p. 18-25.}"
}

@article{fertl1980evaluation,
    author = "Fertl, Walter H. and Frost, Elton",
    title = "Evaluation of Shaly Clastic Reservoir Rocks",
    year = "1980",
    journal = "Journal of Petroleum Technology",
    abstract = "Log-derived spectral gamma ray data have been correlated to core-derived Qv data (i.e., cation exchange capacity per total pore volume) in a Texas coast Tertiary sand, east Texas Jurassic sands, and an Alaskan elastic formation. Such correlations can be used to provide a continuous in-situ water saturation estimate in shaly sands based on the Waxman-Smits equation. Introduction Exceptionally few hydrocarbon-bearing clastic reservoir rocks are essentially free of clay minerals. The significant effect of the latter on important reservoir properties such as porosity, water saturation, and permeability and on most geophysical well log responses is well-established.In clastic reservoirs, various types of clay minerals may occur in dispersed, laminated, or structural form. The types of clay distribution, each with a differing effect on effective porosity, can be inferred from crossplots of well logs, visual study of cores, or detailed SEM investigations. The latter distinguish dispersed-clay occurrences such as discrete particles (patchy kaolinite), pore lining, and pore bridging (illite, chlorite, and smectite), each of which have a pronounced but different effect on reservoir permeability.Clay minerals may be characterized in several ways. Table 1 lists composition, density, hydrogen index, cation exchange capacity C ec, and distribution of potassium, thorium, and uranium based on spectral gamma ray information for some of the more common clay minerals.Furthermore, numerous log-derived clay content (shaliness) indicators are reviewed and discussed (Table 2). These techniques basically assume identical properties for clay present in clastic reservoir rocks and adjacent shales. However, this assumption is often unrealistic.With the advent of the Waxman-Smits model to calculate reliable water saturation in shaly sands, emphasis has been focused on log-derived evaluation of C ec per total pore volume, Qv. The novel application of spectral gamma ray data will be discussed in detail. Water Saturation Calculation Models and Associated Parameters Archie, in his classic empirical equation, relates formation conductivity Ct, formation-water conductivity Cw, and the formation resistivity factor F (a function of porosity phi and cementation exponent m) to the formation-water saturation Sw. Ct =Sw CwF(-1), where F= phi (-m). Archie's equation satisfactorily applies to clean sands. The presence of clay minerals, however, has a detrimental effect on Sw calculations. Since such Sw results are often too pessimistic, several clay/quartz distribution models and Sw calculation concepts have been proposed. JPT P. 1641＾",
    url = "https://doi.org/10.2118/8450-pa",
    doi = "10.2118/8450-pa",
    number = "09",
    openalex = "W2048552318",
    pages = "1641-1646",
    volume = "32"
}

@misc{harms1982structure,
    author = "Harms, J. C. and Southard, J. B. and Southard, J. B. and Walker, R. G.",
    title = "Structure and Sequence in Clastic Rocks",
    year = "1982",
    url = "https://doi.org/10.2110/scn.82.09",
    doi = "10.2110/scn.82.09",
    openalex = "W1755726326"
}

@misc{harms1982structures2,
    author = "Harms, J. C. and Southard, J. B. and Walker, R. G",
    title = "Structures and sequences in clastic rocks",
    year = "1982",
    howpublished = "Society of Economic Paleontologists and Mineralogists, Short Course \#9. Variously paginated",
    note = "talkorigins\_source = {true}; raw\_reference = {Harms, J. C., Southard, J. B., and Walker, R. G., 1982, Structures and sequences in clastic rocks. Society of Economic Paleontologists and Mineralogists, Short Course \#9. Variously paginated.}"
}

@misc{crossref1984late,
    title = "Late Miocene (Santa Margarita Sandstone) shallow marine clastics",
    year = "1984",
    url = "https://doi.org/10.3133/70237219",
    doi = "10.3133/70237219",
    openalex = "W4312841310"
}

@misc{crossref1986modern,
    title = "Modern and Ancient Shelf Clastics",
    year = "1986",
    abstract = "The organizers of this core workshop opted for a broad, permissive definition of shelf clastics and contributors were encouraged to focus on their own interpretations rather than force-fitting their examples to a restrictive theme. As a result, the editors assembled a selection of core examples which range from standline to shelf edge. Given the dominance of petrophysical logs in subsurface studies, contributors to the workshop worked hard to make the necessary core-to-log comparisons which were essential if geologists are to more fully utilize wireline data in facies analysis. Contributors were also encouraged to place their studies within the context of energy prospects associated with environments of deposition. Hydrocarbon potential and reservoir quality dominate these discussions. The high degree of lithofacies variability and the effect of high-energy events on shelf deposits cause sediments formed within this environment to be particularly challenging exploration targets.",
    url = "https://doi.org/10.2110/cor.86.09",
    doi = "10.2110/cor.86.09",
    openalex = "W2479948557"
}

@article{stingl1990sedimentological,
    author = "Stingl, Volkmar and Krois, Peter",
    title = "Sedimentological investigations of metamorphic clastics: the basal clastic rocks of the Brenner Mesozoic (Stubai Alps, Austria/Italy)",
    year = "1990",
    journal = "Terra Nova",
    abstract = "Sedimentological investigations were carried out in the basal clastic rocks of the Brenner Mesozoic in the Stubai Alps. These are Scythian in age and metamorphosed to a greenschist grade. The increase of temperature and pressure from north to south allows the metamorphic effects on Sedimentological features to be gradually traced into higher grade metamorphic areas. The use of various laboratory methods as well as profiling with lithofacies types shows the limitation of using only single methods in sediments suffering thermal and deformational overprint. Only a combined application of different methods allows the extraction of useful sedimentological information. Based on the results of these investigations, a fan delta to shelf succession is proposed for the basal clastic rocks. Petrographic analyses show the relation of the sediments to an underlying weathering horizon.",
    url = "https://doi.org/10.1111/j.1365-3121.1990.tb00075.x",
    doi = "10.1111/j.1365-3121.1990.tb00075.x",
    number = "3",
    openalex = "W2167605841",
    pages = "273-281",
    volume = "2",
    references = "doi1010079781461210665, doi101016001282527990059x, doi1010160169555x91900278, doi101111j136530911963tb01204x, doi1011300091761319808543ncrihs20co2, doi101306212f8e772b2411d78648000102c1865d, doi10130674d711092b2111d78648000102c1865d, openalexw425049407, openalexw572951622, openalexw602333724"
}

@article{annmemarchand12000abstract,
    author = "Ann M.E. Marchand1, R. Stuart Hasze",
    title = "Abstract: Oil Charge Preserves Porosity in Deepwater Clastics",
    year = "2000",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/c9ebdeb3-1735-11d7-8645000102c1865d",
    doi = "10.1306/c9ebdeb3-1735-11d7-8645000102c1865d",
    openalex = "W2331539643",
    volume = "84 (2000)"
}

@incollection{crossref2000clastic,
    title = "Clastic sedimentary rocks",
    year = "2000",
    booktitle = "Exploring Geology on the Isle of Arran",
    url = "https://doi.org/10.1017/cbo9781139168458.008",
    doi = "10.1017/cbo9781139168458.008",
    openalex = "W976883676",
    pages = "33-50",
    references = "doi101016000925419400129v, doi1010160301926888900423, doi101086629071, openalexw2094255421"
}

@article{mcconaughy2001joint,
    author = "McConaughy, David T. and Engelder, Terry",
    title = "Joint initiation in bedded clastic rocks",
    year = "2001",
    journal = "Journal of Structural Geology",
    url = "https://doi.org/10.1016/s0191-8141(00)00091-2",
    doi = "10.1016/s0191-8141(00)00091-2",
    number = "2-3",
    openalex = "W2111482244",
    pages = "203-221",
    volume = "23",
    references = "doi1010160148906294000374, doi101016019181419190085w, doi1010160191814194000588, doi101029jb085ib11p06319, doi10113000167606196778609jitapo20co2, doi10113000167606198394563jfigro20co2, doi1011300016760619881001181piujot23co2, doi1011300091761319940220949iopbot23co2, doi102475ajs2597493, doi102475ajs2638633"
}

@article{liu2012characteristics,
    author = "Liu, ChunYan and Zheng, HeRong and Hu, ZongQuan and Yin, Wei and Li, Song",
    title = "Characteristics of carbonate cementation in clastic rocks from the Chang 6 sandbody of Yanchang Formation, southern Ordos Basin",
    year = "2012",
    journal = "Science China Earth Sciences",
    url = "https://doi.org/10.1007/s11430-011-4352-5",
    doi = "10.1007/s11430-011-4352-5",
    number = "1",
    openalex = "W1973206294",
    pages = "58-66",
    volume = "55",
    references = "doi101007s1011401200306, doi101016jmarpetgeo200409002, doi101111j17457254200500003x, doi101111j175567242008tb00602x, doi1013062dc409160e4711d78643000102c1865d, doi10130661eedabc173e11d78645000102c1865d, doi1013069488787f170411d78645000102c1865d, doi101306a9673b9e173811d78645000102c1865d, doi10136002yd9063, doi102110pec86380123"
}

@article{grundtner2017carbonate,
    author = "Grundtner, Marie-Louise and Gross, Doris and Gratzer, Reinhard and Misch, David and Sachsenhofer, Reinhard F. and Scheucher, Lorenz",
    title = "Carbonate cementation in Upper Eocene clastic reservoir rocks from the North Alpine Foreland Basin (Austria)",
    year = "2017",
    journal = "Austrian Journal of Earth Sciences",
    url = "https://doi.org/10.17738/ajes.2017.0005",
    doi = "10.17738/ajes.2017.0005",
    number = "1",
    openalex = "W2740882115",
    volume = "110",
    references = "doi10100797814684275788, doi1010160016703779900954, doi1010160169555x91900278, doi101016s0009254199000923, doi101038269209a0, doi101111j, doi10113000167606, doi1012019781439833544, doi105860choice301532"
}

@article{doi10130601092623123,
    author = "Wang, Jian and Wu, Bing and Li, Zhenkun and Cao, Yingchang and Yang, Haijun and Wang, Shun and Wei, Hongxiang and Liu, K. and Mo, Tao",
    title = "Differentiation and effect on ultradeep clastic reservoirs of early carbonate cements: Insights from the Cretaceous in Kuqa depression, northwestern China",
    year = "2026",
    journal = "AAPG Bulletin",
    abstract = "ABSTRACT Early carbonate cement is common and widely distributed in clastic rocks and has a complex impact on the quality of clastic reservoirs. At present, although there are studies indicating that early formation of carbonate cement can protect reservoirs to a certain extent, there is no empirical evidence to prove it. Early carbonate is the most abundant cement in the Cretaceous continental ultradeep clastic sandstone in the Kuqa depression. The petrographic characteristics, spatial distribution, and geochemical characteristics of early carbonate cements in the Cretaceous sandstone reservoir are systematically investigated to discuss the origin, distinct distribution, and multifaceted impact on ultradeep clastic reservoirs. During the early Paleogene, meteoric water leached the Paleogene carbonate rocks, providing material for early carbonate cements. Affected by lateral recharge of meteoric water, the vertical recharge of seawater, and the normal-graded sequence, early calcite and dolomite cements with significantly spatial different distribution characteristics were precipitated in the ultradeep clastic reservoirs. Due to the differences in the content and compaction resistance of early calcite and dolomite, their impact on reservoir quality is opposite. Early calcite occupies the reservoir space to varying degrees and has weak compaction resistance, seriously damaging the reservoir quality. Early dolomite has a relatively low content and strong compaction resistance, which can effectively protect the reservoir during deep burial and strong lateral compression processes. This study provides a good example of the positive effect of early carbonate cements on the formation and development of high-quality reservoirs.",
    url = "https://doi.org/10.1306/01092623123",
    doi = "10.1306/01092623123",
    openalex = "W7135098464",
    references = "doi1010029781444304893, doi1010160016703764900225, doi101016jcageo201902011, doi101046j13653091200000007x, doi101086622910, doi1011300016760619891010795rcocci23co2, doi101130g209921, doi101130gsab25655, doi10130601280807107, doi10130604211009178, grundtner2017carbonate"
}

@incollection{crossrefNoneclastic,
    title = "clastic rocks",
    year = "None",
    booktitle = "Dictionary of Gems and Gemology",
    url = "https://doi.org/10.1007/978-3-540-72816-0\_4494",
    doi = "10.1007/978-3-540-72816-0\_4494",
    openalex = "W4231289435",
    pages = "173-173"
}

@incollection{huckenholzNone044,
    author = "Huckenholz, H.-G.",
    title = "0.4.4 Clastic or fragmental sedimentary rocks",
    year = "None",
    booktitle = "Landolt-Börnstein - Group V Geophysics",
    url = "https://doi.org/10.1007/10201894\_15",
    doi = "10.1007/10201894\_15",
    openalex = "W4237495554",
    pages = "50-55",
    references = "doi1010079783642463006, doi10108011035896309448877"
}