Skeletal packstone

22.65–24.65 Lithofacies: Arenaceous skeletal packstone and grainstone Depositional texture: Arenaceous skeletal packstone and grainstone Color: Very pale orange (10YR 8/2) and grayish orange (10YR 7/4) Sedimentary structures/textures: Part of a very thickly bedded interval Ichnofabrics: Ichnofabric index 4–5. Thalassinidean and/or ...

Skeletal packstone. Rim and flank facies include lower slope boundstone breccia mixed with laminated mudstone, volcanic ash, and platform-derived skeletal packstone to grainstone; middle slope poorly-bedded to massive boundstone breccia with sub-types based on clast composition, size, and packing; and upper slope in-situ microbial boundstone.

Skeletal-peloidal wackestone, wacke-packstone, and packstone facies characterize this environment succession. A low-diversity fauna of benthic foraminifera, including miliolids, thin-shelled bivalves, and rare fragmental rudists and green algae characterize the lagoonal environment ( Schlager, 2005 ) with a low-to-moderate energy regime.

252. I tried to make caves more effective and here is the most basic level of the skulls on stones pack. If you have any idea that improves Vanilla feeling, feel free to …are Skeletal Packstone, Red Algae Packstone, Foram Packstone, and Boundstone with diagenetic environment Mixing Zone, Fresh Water Phreatic, and Meteoric Vadose. Porosity, permeability defined by ...Benthic Foraminifera. 1. Fusulinid and Textularid. Skeletal grainstone with cross-sections of beresellid algae and two well preserved specimens of the textularid foraminifer Climacammina (centre left) and Bradyina (top right) …Apr 25, 2019 · The western and central parts of the outcrop are dominated by coral framestone. Towards the east, a transition to coral-skeletal rudstone and algal-foraminiferal-skeletal packstone can be observed. In the upper part of the outcrop, gastropod-skeletal packstone is followed by blocks of coral-algal rudstone. The Gigantoproductus skeletal grainstone also occurs at 9.25 – 9.75 m, separated from the lower bed by the crinoidal packstone and wackestone. At the top of the section, size grading of crinoid ossicles indicates turbulent current allowed significant sorting during deposition of the skeletal packstone–wackestone with intraclasts.The skeletal system works constantly with the muscular system, and the circulatory system, endocrine system and integumentary system also have interactions with it. The skeletal system provides vital support and protection for all the other...Wherein, Upper Tomori Formation is composed of planktic-large foram packstone-wackestone with deposited Middle-Outer Sublittoral and skeletal packstone-wackestone with deposited Inner-Middle ...Download scientific diagram | Normal marine subtidal facies: (a) smaller foraminiferal packstone-grainstone (BD), Korobcheevo Formation, Podolsk; (b, c) skeletal packstones-rudstones (D1): (b ...

Condensed skeletal packstone with a transversal cross section of gastropod (with geopetal filling) coated by Archaeolithophyllum lamellosum. Pennsylvanian, Asturias, N Spain, cf. Bahamonde et al. (2015, 2017) HIDE INFO. SHOW INFO. 4. Palaeozoic red algae . Skeletal packstone with growth of possible red alga Fasciella and green algae beresellidsThe MFS is at the base of the non-fossiliferous lime mudstone containing abundant wispy kerogenous laminae in more basin-central positions. Locally, this mudstone rests on thin skeletal packstone sheet or thicker skeletal wackestone-floatstone. Updip, the MFS is at the base of laminated dolomite that occurs on top of a thin skeletal packstone.Petrographic analysis shows a leached skeletal packstone texture. Evidence of leached pelloidal matrix is observed, along with unidentified skeletal grains and fragments.Download scientific diagram | Non-poor reservoir lithofacies type 24: Burrowed, bioturbated, skeletal packstone (BBSP). Core photograph shows undifferentiated burrowing. Thin-section ...– Fasies skeletal packstone & wackestone; terletak di bagian timur, dan diinterpretasikan sebagai reef front-fore reef. Fasies ini memiliki porositas sekunder (vuggy & moldic) yang berkembang dengan baik. – Fasies coral & algal boundstone; diinterpretasi-kan sebagai reef core. – Fasies lime mudstone; terletak di sisi baratA skeletal building structure is a steel frame that is built to support a large building or skyscraper. The structure consists of metal beams forming vertical columns crossed with steel girders for stability.252. I tried to make caves more effective and here is the most basic level of the skulls on stones pack. If you have any idea that improves Vanilla feeling, feel free to …

Jul 16, 2015 · Carbonate reservoir geology. Carbonate sediments are commonly formed in shallow, warm oceans either by direct precipitation out of seawater or by biological extraction of calcium carbonate from seawater to form skeletal material. The result is sediment composed of particles with a wide range of sizes and shapes mixed together to form a ... Abstract. In the Lower Cambrian of southwest Sardinia, a carbonate platform developed, showing clearly different stages of evolution: (1) a homoclinal ramp containing algal-archaeocyathan mounds (consisting mainly of Epiphyton and Renalcis boundstone) in the west, clastic tidal flats in the east; (2) an ooid-pellet barrier ramp with ooid-shoals, prograding toward the west.Packstone. A Packstone: grain supported by small grains (width of picture is 7mm) Under the Dunham classification (Dunham, 1962 [1]) system of limestones, a packstone is defined as a grain-supported carbonate rock that contains 1% or more mud-grade fraction. This definition has been clarified by Lokier and Al Junaibi (2016) [2] as a carbonate ... It is composed of regularly occurring scoured skeletal wackestone–packstone sheets (LF10) (Fig. 7b) and intervening mudstones (LF3). Skeletal sheets are characterized by fining-up sequences of molluscs, crinoids, brachiopods gastropods, forams and intraclasts that lay above a scoured sole (Fig. 7c). Large crinoids and lithoclasts often fill ...

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Hasil analisa fasies yang ada pada daerah penelitian adalah terdapat 5 fasies,yaitu; Skeletal Debris Packstone – Wackestone, Coral Algal Grainstone - Boundstone,Skeletal Wackestone, Skeletal Packstone dan Coral Algal Packstone. Fosil yangterdapat pada daerah penelitian ini di dominasi oleh coral, red algae, molusca,bryozoans, bivalve ...are Skeletal Packstone, Red Algae Packstone, Foram Packstone, and Boundstone with diagenetic environment Mixing Zone, Fresh Water Phreatic, and Meteoric Vadose. Porosity, permeability defined by ...If the limestone also contains a minor element such as skeletal fragments, then it is called a skeletal-oolitic limestone. Two of the most widely used classifications are those of Folk (1959,1962) and Dunham (1962). Both classifications subdivide limestone s primarily on the basis of matrix content.Skeletal peloidal packstone (F8) includes bivalves, gastropods, foraminifera (aulotortids, duostominids, textulariids, Triasina hantkeni), and dasyclad algae (Fig. 6H). Bioturbated packstone with moulds of ooids with peloids as nuclei characterises lithofacies F9 (Fig. 7 A).Skeletal grainstone/packstone. This is a more common rock type and consists of dasycladacean green algae (e.g., Clypina jurassica), a characteristic fossil of the Arab Formation all over eastern Arabia (Sadooni 1997), with stromatoporoids, sponges, benthonic foraminifera, echinoderms, and gastropods.

Skeletal Grain types | Images | Gastropods ATLAS INDEX Skeletal Grain types Terminology Images Gastropods 1. Gastropod Skeletal peloidal grainstone with sparse …The MFS is at the base of the non-fossiliferous lime mudstone containing abundant wispy kerogenous laminae in more basin-central positions. Locally, this mudstone rests on thin skeletal packstone sheet or thicker skeletal wackestone-floatstone. Updip, the MFS is at the base of laminated dolomite that occurs on top of a thin skeletal packstone.Download scientific diagram | Photomicrographs of carbonate microfacies (all in plane polarized light) of early to late Viséan limestones. A–Skeletal packstone with closely packed bioclasts ...D) Close-up of the breccia interval; large clasts consist of various lithofacies (pelagic lime-mudstone, calciturbiditic grainstone to packstone) and the matrix varies from rudstone to floatstone.3. Peloids . Peloidal (micritic elliptical grains and micritized bioclasts) skeletal (foraminifera Archaias) grainstone to packstone with peloids due to sea floor micritization activity by endolithic micro-organisms (lagoon, modern carbonate settings).. Bahamas, Holoceneskeletal packstone-grainstone, fusulinid-peloid packstone). Outer-ramp fusulinid-peloid wackestone and packstone. Undifferentiated inner-ramp, ramp-crest ...The observed lithofacies are (1) foraminiferal and skeletal debris wackestone-packstone, (2) coral float-stone-rudstone, and (3) algal and skeletal wackestone-packstone; and microfacies are (1 ...The base of the overlying Chote č Limestone begins in the costatus Zone and is characterized by a ~1 m-thick interval of dark, graded peloidal – skeletal grainstone – packstone (turbidites ...Type of skeletal and non-skeletal grains, grain size and their frequency ... packstone, Operculina bioclast packstone and Lepidocyclina bioclast packstone.This is overlain by a skeletal peloid mudstone to packstone, with minor intercalated mollusk rudstone beds (Figs. 13 and 14). Updip in core SC-4, the TST of Md 5 is a deepening upward succession of sand to lagoonal carbonates then up into seagrass bank skeletal packstone (Fig. 12). Downdip, (SC-1) it consists of a thin sand up into a lagoonal ...

... packstone, wispy-laminated crinoid packstone, and skeletal packstone-grainstone. ... Skeletal packstones and grainstones. ANHYDRITE-DOLOMITE ASSOCIATION AND ...

Skeletal and shelly debris, ranging from largely articulated to disarticulated, is common in the Dumugol reefs. The debris occurs commonly in bioclastic wackestone …Details: The base of the member is a thin (few centimeters) skeletal packstone layer, rich in inarticulate brachiopod (obolids) shell hash and trilobite cuticle fragments (Fortey and Bruton, 1973). The horizon has been found at section FP and in several places along the Profilbekken River, where it was impossible to reconstruct a …The dolomitic part of K1 is characterized to be mudstone, mudstone to packstone, beige, moderately hard to hard, crystalline to cryptocrystalline, have occasional pelloids, pebbles and shell fragments, have local mudcracks in mudstone, slightly argillaceous in parts, have thin layers of anhydrite and o have good to fair vuggy and ...Abstract. During the past three years the attention of Rocky Mountain operators has been focused on Permian-Pennsylvanian reservoirs in the Nebraska Panhandle. Relatively inexpensive drilling, a good wildcat success ratio, and impressive oil production have made the Northern Denver one of the most active areas in the Rockies during the current ...By far the most-dominant carbonate grain type in the Trenton Limestone, skeletal fragments from echinoderms, arthropods such as trilobites and ostracodes, bryozoans, brachiopods, molluscs, sponges etc. make up significant portions of these limestones.G) Mixed skeletal and foraminiferal fragments in the skeletal/foram packstone facies. H) Dasyclad algae and Tubiphytes in the foram/algal packstone facies. I) Peloidal packstone facies.Note its massive body and surrounding deposits of intraclastic-skeletal packstone to grainstone (P/Gi) and overlying facies of differentially compacted mudstone with dissolution seams (Md).Peloidal–skeletal packstone to grainstone (L1) was deposited before the onset of the mud mound complex in a moderate-energy, subtidal, open-marine inner-ramp setting, as suggested by the abundance of peloids, bioclasts, and endothyrid foraminifers (Gallagher 1988; Della Porta et al. 2005).However, the microbial-laminated peloid-skeletal packstone grades laterally (location 1: vertical section MC-1; Figures 2 and 3a) and vertically (location 1a and location 2: vertical section MC-2; Figures 2, 6 and 7a) into a peloid-skeletal packstone with rootlets. This favors the interpretation of lateral facies variations or short term sea ...They are 5–10 m thick and consist of nodular, very fine to medium grained, skeletal fragment packstone–wackestone (with scattered large forams) and rarely mudstone, capped by larger foram packstone–rudstone, or higher in the section, by shallow water, coarse to very coarse, skeletal fragment grainstone–packstone with sea grass …

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Fragmented and abraded skeletal wackestone to packstone (MS3)4.1.3.1. Description. Facies MS3 is composed of ≤1.5-m-thick beds of wackestone to packstone that are primarily composed of fragmented and variably abraded (angular to sub-rounded) skeletal grains ranging from silt- to granule-size (Fig. 6 C). Individual beds preserve a …Download scientific diagram | Guadámez 2 column and field aspects of selected levels. a) View of the upper part of unit 8 and units 9 to 13. b) View of the units 15 to 17. c) View of the upper ...(C) Mud-rich packstone that is rich in deformed micritized allochems; note that partial early calcite cementation has preserved some peloids from being deformed locally (D) A cross plot of core plug porosity (%) and permeability (mD) of different limestone textures, data comes from the Arab and Kharaib formations (this study) and Thamama ...Based on lithology and stratal patterns, four facies groups have been recognized: (1) a flat-topped platform, in which thick algal boundstone, skeletal packstone–grainstone and peloidal micrite wackestone with a poorly rhythmic character prevail; (2) the platform margin and upper slope, characterized by microbial boundstone spanning a ...... packstone, wispy-laminated crinoid packstone, and skeletal packstone-grainstone. ... Skeletal packstones and grainstones. ANHYDRITE-DOLOMITE ASSOCIATION AND ...d. Crystal precipitation during the evaporation of water, such as in a drying lake bed. 13. Sample G is: a. rock gypsum b. chert c. mudstone/shale d. quartz sandstone e. skeletal packstone/coquina f. conglomerate 14. Sample H is: a. rock gypsum b. chert c. mudstone/shale d. quartz sandstone e. skeletal packstone/coquina f. conglomerate 15.... packstone, wispy-laminated crinoid packstone, and skeletal packstone-grainstone. ... Skeletal packstones and grainstones. ANHYDRITE-DOLOMITE ASSOCIATION AND ...Abstract. During the past three years the attention of Rocky Mountain operators has been focused on Permian-Pennsylvanian reservoirs in the Nebraska Panhandle. Relatively inexpensive drilling, a good wildcat success ratio, and impressive oil production have made the Northern Denver one of the most active areas in the Rockies during the current ... ….

Skeletal packstone with foraminifera and peloids with a several mms long gastropod in longitudinal section. The gastropod shell exhibits geopetal filling and an oncoidal coating by the alga Archaeolithophyllum lamellosum and micrite crusts. Pennsylvanian, Asturias, N Spain, cf. Bahamonde et al. (2015, 2017) ...Stratigraphically, Yamama Formation represents the regressive carbonate cycle comprising the neritic lithofacies of the cycle. Three depositional cycles included within Yamama Formation, top cycle comprises inner ramp facies (oolitic grainstone), middle-ramp (packstone, wackestone), and the third bases cycle outer ramp (chalky micrite and gray …(A) Skeletal packstone with preserved fenestellid bryozoan (by), Tetrataxis foraminiferan (f) and crinoid ossicle (cr) (sample 1a, taken at height c. 1.25 m from the base of the …Figure 13. Weathering characteristics of a dolomitized wackestone-packstone .....37 Figure 14. Weathering properties of a coarse-grained skeletal packstone .....38 Figure 15. Joints and solution features in the upper part of the ACR section.....39 Figure 16.The peloids and non-skeletal grains showed less alteration, and the thickness of any margin rim of brown color was less significant. At the King Abdullah Economic City site, the beach contained a mix of non-skeletal and skeletal carbonate sands (Table 1; Electronic supplementary material, ESM, Table S1). Corals, red algae, and mollusks form …Wackestone to Packstone . Micrite matrix-supported to locally grain-supported (due to bioturbation) with micrite matrix between the grains; skeletal grains (upper Cretaceous planktonic foraminifera) > 10%. Thin section kindly provided by T. Geel, Vrije Universiteit, Amsterdam . HIDE INFO ...Nov 1, 2021 · Skeletal packstone–floatstone (SPF) Gray skeletal packstone to floatstone with visible fine sand-sized carbonate grains. In hand sample, facies SPF beds are more visibly grainy than the purple lime mudstone facies and contain a range of large skeletal clasts from 0 to 20%. Weathers to a tan color similar to facies HSP (Fig. 6 B). The skeletal grainstone/packstone lithofacies (lithofacies 4) is composed of very fine skeletal grains with many peloidal grains and some very-fine quartz and fine ooid grains (figure 5). This lithofacies is greenish to dark yellowish-brown color, and contains variable amounts of relatively unabraded skeletal fragments.Packstone textures prevail although oncoidal grainstones and wackestones occur. Oncoid abundances range from 12 to 75%. Other skeletal grains include whole to ...sive skeletal packstone to rudstone containing abun-dant large crinoids and bra-chiopod fragments, minor colonial coral detritus, and occasional platform-derived breccias. In the central plat- Skeletal packstone, The microfacies, from selected outcrops from the Åland Islands, Finland and Estonia, consists of calcareous green algae as the main skeletal component in a …, The first occurrence (FO) of H. parvus parvus in the lower Daye Formation, at about 7.45 m above the contact surface between the Upper Permian skeletal packstone and a calcimicrobial framestone ..., Bioclastic crinoidal packstone. 658 views · 2 years ago ...more. Try YouTube Kids. An app made just for kids. Open app · Scienze della Terra - La Statale. 761., burrowed/laminated chert, and (4) skeletal packstone (Ruppel and Holtz, 1994; Ruppel and Barnaby, 2001) . Dark-colored, abiotic, chert/carbonate laminites (fig. 6a) constitute basal Thirtyone deposits in the thickest parts of the basin, where they typically overlie carbonate mudstones and shales of the Silurian-Devonian Frame Formation (fig. 4)., Marginal lacustrine deposits include ooid and skeletal packstone-grainstone, siltstone, and sandstone. Distal lacustrine units are skeletal mudstone ..., 3. Peloids . Peloidal (micritic elliptical grains and micritized bioclasts) skeletal (foraminifera Archaias) grainstone to packstone with peloids due to sea floor micritization activity by endolithic micro-organisms (lagoon, modern carbonate settings).. Bahamas, Holocene, Skeletal Grain types | Images | Gastropods ATLAS INDEX Skeletal Grain types Terminology Images Gastropods 1. Gastropod Skeletal peloidal grainstone with sparse …, TSTs of Sequences Md 1 to 5 downdip are carbonate-prone, with parasequence sets becoming progressively more open-marine upward from peloid …, Sample Kis: a. rock gypsum a. rockert c. mudstone/shale d. quartz sandstone c. skeletal pneksten f. conglomerate 18. Sample L is: a. rock gypsum b. chert c. mudstone/shale d. quartz sandstone e. skeletal packstone/coquins f. conglomerate 19. Search for 61420 S 293058 E and zoom out to an cye altitude of − 600 milles. What type of sedimentary ... , Marginal lacustrine deposits include ooid and skeletal packstone-grainstone, siltstone, and sandstone. Distal lacustrine units are skeletal mudstone ..., Skeletal grainstone/packstone. This is a more common rock type and consists of dasycladacean green algae (e.g., Clypina jurassica), a characteristic fossil of the Arab Formation all over eastern Arabia (Sadooni 1997), with stromatoporoids, sponges, benthonic foraminifera, echinoderms, and gastropods., Description It was named formerly mollusk packstone (Alkhaldi 2009) and massive peloidal skeletal packstone (Bashri et al. 2017).This is the basal facies …, Quartz sandstone Shale Limestone G H Crystalline limestone Skeletal packstone (?) Rock gypsum K *these rocks are not the in the choices. 2 Attachments. png. png. View answer & additonal benefits from the subscription Subscribe. Related Answered Questions. Explore recently answered questions from the same subject ..., The MFS of sequence 4 cannot be picked lithologically to the south on the arch, but in the north it probably occurs within the tongue of nodular skeletal packstone and shale that onlaps the ..., From its base upsection, the formation is mostly subtidal in origin and emergent at its top, and consists of (1) deeper water carbonates, (2) major cycles of open shallow-marine mudstones grading up into skeletal packstone or rainstone, (3) minor cycles of dolomitized transitional open to restricted marine mudstone grading up into skeletal ..., Stratigraphically, Yamama Formation represents the regressive carbonate cycle comprising the neritic lithofacies of the cycle. Three depositional cycles included within Yamama Formation, top cycle comprises inner ramp facies (oolitic grainstone), middle-ramp (packstone, wackestone), and the third bases cycle outer ramp (chalky micrite and gray …, Packstone and grainstone both consist mostly of carbonate grains, but differ in that packstone has a carbonate mud matrix while grainstone has carbonate cement between the grains. It is difficult to consistently distinguish between wackestone and packstone and is not important to make the distinction, so lump these two rock types together as ..., 1. Packstone. Grain-supported; carbonate mud matrix between skeletal grains (dasyclad algae, benthic foraminifers, bivalves) in interparticle pore space. Thin section kindly provided by T. Geel, Vrije Universiteit, Amsterdam. HIDE INFO. , Nov 1, 2016 · The MFS is at the base of the non-fossiliferous lime mudstone containing abundant wispy kerogenous laminae in more basin-central positions. Locally, this mudstone rests on thin skeletal packstone sheet or thicker skeletal wackestone-floatstone. Updip, the MFS is at the base of laminated dolomite that occurs on top of a thin skeletal packstone. , 28 BAB IV HASIL DAN PEMBAHASAN Data yang digunakan dalam penelitian analisa fasies dan lingkungan pengendapan pada lapangan “Jannah” yang terletak pada daerah Utara Bali, terdiri, Medicine Matters Sharing successes, challenges and daily happenings in the Department of Medicine ARTICLE: Exercise intolerance and rapid skeletal muscle energetic decline in human age-associated frailty AUTHORS: Sabra C. Lewsey, Kilian Wei..., Sample Kis: a. rock gypsum a. rockert c. mudstone/shale d. quartz sandstone c. skeletal pneksten f. conglomerate 18. Sample L is: a. rock gypsum b. chert c. mudstone/shale d. quartz sandstone e. skeletal packstone/coquins f. conglomerate 19. Search for 61420 S 293058 E and zoom out to an cye altitude of − 600 milles. What type of sedimentary ... , Abstract. ABSTRAK Lokasi Lapangan ‘P’ adalah lapangan migas PT. PERTAMINA EP ASSET 4 yang terletak di Kab. Tuban. Daerah telitian secara stratigrafi termasuk ke dalam Formasi, The base of the overlying Chote č Limestone begins in the costatus Zone and is characterized by a ~1 m-thick interval of dark, graded peloidal – skeletal grainstone – packstone (turbidites ..., Nov 1, 2016 · The MFS is at the base of the non-fossiliferous lime mudstone containing abundant wispy kerogenous laminae in more basin-central positions. Locally, this mudstone rests on thin skeletal packstone sheet or thicker skeletal wackestone-floatstone. Updip, the MFS is at the base of laminated dolomite that occurs on top of a thin skeletal packstone. , Embry and Klovan modification of the Dunham’s (1962) biologic classification of organically bound rocks.“Floatstone” replaces Dunham’s “packstone”; the term “rudstone” replaces grain-supported biogenic limestones, and other organically bound rock are termed “bafflestone,” “bindstone,” or “framestone,” depending on the character of the organic …, Note its massive body and surrounding deposits of intraclastic-skeletal packstone to grainstone (P/Gi) and overlying facies of differentially compacted mudstone with dissolution seams (Md)., May 19, 2005 · The skeletal grainstone/packstone lithofacies (lithofacies 4) is composed of very fine skeletal grains with many peloidal grains and some very-fine quartz and fine ooid grains (figure 5). This lithofacies is greenish to dark yellowish-brown color, and contains variable amounts of relatively unabraded skeletal fragments. , Most parasequences are made up of basal skeletal-peloid wackestone-packstone that grades up into a thick skeletal packstone-grainstone (Fig. 9 F), capped by a thin microbial or fenestral laminite. The parasequences in the 300-m-thick Oxfordian-basal Kimmeridgian part of the DJ section are dominated by mud-supported facies and vary widely in ..., 3. Peloids . Peloidal (micritic elliptical grains and micritized bioclasts) skeletal (foraminifera Archaias) grainstone to packstone with peloids due to sea floor micritization activity by endolithic micro-organisms (lagoon, modern carbonate settings)., d. Crystal precipitation during the evaporation of water, such as in a drying lake bed. 13. Sample G is: a. rock gypsum 12 b. chert c. mudstone/shale d. quartz sandstone e. skeletal packstone/coquina f. conglomerate 14. Sample H is: a. rock gypsum b. chert c. mudstone/shale d. quartz sandstone e. skeletal packstone/coquina f. conglomerate 15., 22.65–24.65 Lithofacies: Arenaceous skeletal packstone and grainstone Depositional texture: Arenaceous skeletal packstone and grainstone Color: Very pale orange (10YR 8/2) and grayish orange (10YR 7/4) Sedimentary structures/textures: Part of a very thickly bedded interval Ichnofabrics: Ichnofabric index 4–5. Thalassinidean and/or ..., Hasil analisa fasies yang ada pada daerah penelitian adalah terdapat 5 fasies,yaitu; Skeletal Debris Packstone – Wackestone, Coral Algal Grainstone - Boundstone,Skeletal Wackestone, Skeletal Packstone dan Coral Algal Packstone. Fosil yangterdapat pada daerah penelitian ini di dominasi oleh coral, red algae, molusca,bryozoans, bivalve ...