Electron microscope analysis of zoned dolomite rhombs in the. A basal bird from the campanian late cretaceous of. Unfortunately, existing summaries of the lower lias succession compiled for the severn basin e. Assessment of groundbased monitoring techniques applied to. Contrasting watermass conditions during deposition of the. A landslide complex in the whitby mudstone formation at hollin hill, north yorkshire, uk is periodically reactivated in response to rainfallinduced porewater pressure fluctuations. The mercia mudstone group is an early triassic lithostratigraphic group a sequence of rock strata which is widespread in britain, especially in the english midlands the name is derived from the ancient kingdom of mercia which corresponds to that area. This is a medium and dark grey fossiliferous mudstone and siltstone, laminated and bituminous in part, with thin siltstone and silty mudstone beds and rare finegrained calcareous sandstone beds. Whitby mudstone formation at staithes in north yorkshire. Note the size of the exposed rock face, and the heap of earth and stone at its base. In downward sequence they are the main, pecten, two foot, raisdale and avicula seams, the last one, in this. Robinson over a period of seventeen years from 1951 to 1968. The overall strategy of 2f2s is built around the knowledge that efficient predictions of producibility of tough gas plays, such as gas shales, tight.
Impact of water saturation on the elastic anisotropy of the. Rapid observations to guide the design of systems for long. The impact of global warming and anoxia on marine benthic. Topsoil consisting of medium dense dark brown sand and stiff orange brown clays with varying proportions of gravel including sandstone and quartzite and extended to a maximum depth of 0. Ultrasonic velocity and attenuation anisotropy of shales. The rock fall, probably unfairly, was blamed on the roseberry ironstone mine workings under the summit. Microstructural characteristics of the whitby mudstone formation uk. Geotechnical properties of a weak mudstone in downtown calgary. The taxonomy and systematics of parapsicephalus purdoni. Landsliding at hollin hill in north yorkshire, uk is complex and continuing, and includes shallow, retrogressive rotational failure on the upper slope, translation, and flow from the base of the whitby mudstone formation over the scarp slope of the staithes sandstone formation. This observation is consistent with the lack of normal faulting at saltwick nab, and the whitby mudstone formation having been drained by structural and. The elemental geochemistry data were used to assess the palaeoredox state of the depositional environment, the role of dilution of organic matter by siliciclastic material, and the rates of organic productivity in the photic zone above the site of deposition. Whitby mudstone charmouth mudstone tile hill mudstone. The taxonomy and systematics of parapsicephalus purdoni reptilia.
The staithes sandstone formation is also visible above. Whitby mudstone formation wmf is a finegrained mudstone with siltsized minerals embedded in a finegrained matrix, which is microstructurally comparable to the psf. It can be a very productive location when the conditions are right, yielding a wide range of ammonite species. Horizontal fracturefault network characterization of. Appendix 3 soiltechnics soil permeability test report. The uppermost staithes sandstone formation to lowermost alum shale member were studied in a core drilled recently approximately 10 km south of whitby and 7 km west of robin hoods bay to investigate the evolution of pliensbachiantoarcian lower jurassic depositional environments of the cleveland basin, yorkshire, uk. Lias group engineering geological studies of bedrock formations. Pdf whitby mudstone formation its microstructure, porosity and. The whitby mudstone formation is predominantly argillaceous and locally c. Mudstone finely laminated, basinal sediments of the devonian swan hills formation, western canada.
The quarry exposes a full sequence of the marlstone, 3. Engineering geology of british rocks and soils lias group. The wmf section can be subdivided in a carbonate fossil rich upper and a carbonate poor. It has been associated with fossils for hundreds of years. Microstructural controls on the uredependent press. The northampton sand is classified as a minor aquifer, whilst the whitby mudstone is likely to be a nonaquifer. Bedparallel fractures have not been observed within more rich units at the top of the whitby mudstone formation at whitby east cliff, or within wellbedded, clayrich shale at saltwick nab. The pliensbachiantoarcian early jurassic fossil record is an archive of natural data of benthic community response to global warming and marine longterm hypoxia and anoxia. Notable features, as seen in the illustration to the right, are well bedded coarser sandstones alternating with finer sediments where the bedding has been destroyed due to bioturbation. A combined geomorphological and geophysical approach to. Microfabric, mineralogy and early diagenetic history of the. The seams, as seen in the illustration to the left, are clearly visible, usually being coated in a white clay mineral, probably dickite. They tiny particles settle to the bottom of oceans, lake floors or lagoons or even in quiet stretches of rivers.
Terms such as claystone and siltstone are often used in place of mudstone, although these refer to rocks whose grain size falls within much narrower ranges and under close examination these are often technically mudstones. Northampton sand formation consisting of medium and high strength light brown orange sandy clay and. A photographic guide siri scientific press more than 200 colour photographs and illustrations photography by benjamin hyde and illustrations by nobumichi tamura the small coastal town of whitby is located in north yorkshire, england. This is another location where you can find ammonites and shells. The whitby mudstone and alum shales are exposed on the highest part of the shore and at the foot of the cliff. Above the ssf is the cleveland ironstone formation cif, so named because of the ironstone seams which were once quarried or mined. Microfabric, mineralogy and early diagenetic history of. Mudstone, dark grey, bituminous and pyritic, with common layers of grey calcareous concretions, ovoid and spherical and ranging up to 4. Rotunda geology group the robinson ammonite collection. Carbonates are only one of the types of chemical sedimentary rocks. Download the pdf of engineering geology of british rocks and soils. The fractured and highly fissile nature of weak mudstone renders block sampling and preparation of specimens unusually. Mudstone is made up of finegrained clay particles mudstone is called shale.
The wilmcote limestone is absent to the east of the axis in southernmost and southeastern warwickshire ambrose, 2001. A more likely cause was the period of heavy rain immediately prior to. A new sauropod dinosaur from the middle jurassic of the. The mulgrave shale member of the whitby mudstone formation can microstructurally be subdivided into a fossil rich 15% upper half and a submm mineralogically laminated lower half. Microstructural characteristics of the whitby mudstone. A fragmentary bone from the dinosaur park formation campanian of dinosaur provincial park alberta, canada, originally described as a pterosaur tibiotarsus, is reinterpreted as the distal end of the tibiotarsus of a basal bird, probably an enantiornithine, on the basis of several distinctive characters. The staithes sandstone formation ssf consists of shallow marine sandstones and siltstones. Whitby mudstone formation from the cleveland basin using the then recent development of backscattered scanning electron microscopy.
A new record of a sauropodomorph dinosaur is here described from the middle jurassic aalenian saltwick formation of whitby yorkshire, uk. Mudstone formation hettangianpliensbachian underlies the whitby mudstone formation, and is extensively exposed at robin hoods bay. Martill2 1,2school of earth and environmental sciences, university of portsmouth, burnaby building, burnaby road, united kingdom, po1 3ql. Inorganic geochemistry and palaeoenvironments of the early. The wmf is the lateral equivalent of the psf in northen europe ghadeer et al. Nov 15, 2000 read contrasting watermass conditions during deposition of the whitby mudstone lower jurassic and kimmeridge clay upper jurassic formations, uk, palaeogeography, palaeoclimatology, palaeoecology on deepdyve, the largest online rental service for scholarly research with thousands of academic publications available at your fingertips.
Medium and dark grey fossiliferous mudstone and siltstone, laminated and bituminous in part, with thin siltstone or silty mudstone beds and rare finegrained calcareous sandstone beds. Minor fault in the cropwell bishop and blue anchor formations of the mercia mudstone at cropwell bishop, nottinghamshire. Durham etheses inorganic geochemistry and palaeoenvironments. The whitby mudstone is an analogue for the dutch posidonia shale which is a possible unconventional source for gas. Some geologists designate as mudstone any similar rock that is blocky or massive. Microfabric, mineralogy and early diagenetic history of the whitby mudstone formation toarcian, cleveland basin, u. We then describe the lithostratigraphy of the cleveland ironstone and whitby mudstone formations, and present observations of faults and fractures within the cleveland ironstone formation at jet wyke, and the whitby mudstone formation at port mulgrave, whitby east cliff and saltwick nab. Cornbrash cbr whitby mudstone formation whm long nab lon cleveland ironstone formation cdl. Electron microscope analysis of zoned dolomite rhombs in the jet rock formation lower toarcian of the whitby area, u. A single caudal vertebra represents an early sauropodomorph and signifies the earliest recognised eusauropod dinosaur from the united kingdom. The formation, part of the lias group, is present in the. Geotechnical properties of a weak mudstone in downtown. Cowbar nab is the type locality for this formation.
Mudstones form when very finegrained clay particles are deposited in water. As the mud is buried and compacted by overlying sediment, the water is squeezed out and it turns into mudstone. Bedparallel fractures have not been observed within more formula rich units at the top of the whitby mudstone formation at whitby east cliff, or within wellbedded, clayrich shale at saltwick nab. Triaxial deformation tests were performed on mudstone core plugs to investigate the impact of water saturation on the elastic anisotropy of the whitby mudstone united kingdom. Investigation of suspected gulls in the jurassic limestone. Mudstone, sedimentary rock composed primarily of clay or siltsized particles less than 0. The elastic anisotropy of mudstones is not well understood because of their complex nature and the lack of laboratory experiments performed on wellpreserved samples. It is composed of mudstones and sandstone, usually with abundant plant debris. The formation, part of the lias group, is present in the cleveland and worcester basins and the east midlands shelf.
The wmf section can be subdivided in a carbonate fossil rich upper and a carbonate poor sub mm scale mineralogically layered lower half. In the early toarcian mean temperatures increased by the same order of magnitude. The whitby mudstone formation has one of the highest landslide densities in the uk with 42 landslides per 100 km 2. Both formations are deposited during the lower jurassic toarcian, roughly under the same anoxic sedimentary conditions. As the harford member is characterized by poorly compacted sandstone and a thin layer of mudstone 0.
Model metadata report for hs2 area 4 geology and regional geophysics programme open report or15035. Using active ultrasonic source survey data, codawave decorrelation cwd timelapse imaging during the triaxial compression of whitby mudstone cores provides a 3d description of the evolution and redistribution of inelastic strain concentrations. The mineralogy of mudrocks from the lias group of england. Stratigraphical summary of the permian in part, triassic, jurassic and cretaceous rocks and quaternary deposits in. To the west of staithes, the redcar mudstone formation can be seen in the cliff face. Determination of reactions and integrity of cement mudstone interfaces a thesis submitted to the university of manchester for the degree of master of science in the faculty of physical sciences 2016 jorge arturo mendoza ulloa school of earth, atmospheric and environmental sciences. The grantham formation is a geological formation in england, which dates to the middle jurassic aalenian age around 172 million years ago. These contain fossil wood and pyritic mudstone, which is full of poor grade crushed jet and the small bivalve, dacryomya ovum. Mudstone mudstone is an extremely finegrained sedimentary rock consisting of a mixture of clay and siltsized particles. Appendix 2 list of formations in alphabetical order with preferred. The upper lias whitby mudstone formation having as many as 42. The mudstone samples were recovered from the deep excavation for the bow office tower located in the heavily builtup area of downtown calgary. Elsewhere, at base of mudstone overlying ironstone of the marlstone rock formation. Pdf whitby mudstone formation its microstructure, porosity.
Mercia mudstone group engineering geological studies of. The nearest controlled surface water receptor is the brampton branch of the river nene, located approximately 350m to the west of the site. Other highlights include a well preserved succession of biostratigraphical horizons within the cleveland ironstone and the most complete toarcian succession in britain represented by the whitby mudstone formation. Above this are the cement shales, overlain by the dogger and saltwick formations. It is frequently encountered in older literature as the keuper marl or keuper marl series the mercia mudstone group is now. In most areas, sharp, eroded boundary with limestones or sandstones of the inferior oolite group east midlands shelf or the ravenscar group or dogger formation cleveland basin. We have conducted ultrasonic experiments, between 0.
The mercia mudstone group is an early triassic lithostratigraphic group a sequence of rock strata which is widespread in britain, especially in the english midlands indeed the name is derived from the ancient kingdom of mercia which corresponds to that area. Natural fractures in a united kingdom shale reservoir analog. Plot of standard penetration test spt n value against depth for mudstones of the mercia mudstone group. The blg file needed to be deduplicated and the borehole filter tool was used to address.
Request pdf microstructural characteristics of the whitby mudstone formation uk when trying to improve gas productivity from unconventional sources a. Horizontal fracturefault network characterization of pavement. The whitby mudstone is a toarcian geological formation in yorkshire and worcestershire, england. Whitby mudstone formation 30 20 cleveland ironstone formation not available 16 redcar mudstone formation 230 70 on the basis that 96% of the materials to be stored onsite are to at lady cross comprise redcar mudstone, the average leachability concentration for those strata has.
Outcrops of the lower lias group also occur near staithes howarth, 2002. Howarth 1962, consisting of medium to dark grey, flakey. New, wellpreserved examples of the linguliform brachiopod discinisca holdeni are reported from the belemnite marl and green ammonite members of the lower jurassic charmouth mudstone formation, near golden cap, dorset. Whitby mudstone formation late early jurassic toarcian 5 subdivisions, mostly muddy common features sediments finely laminated, dark grey mudstones. The strict application of the definition of the blue lias formation, currently taken at the top of the highest limestone in an interbedded mudstone limestone succession, would include beds previously classified as shaleswithbeef in east devon. New information on hauffiosaurus reptilia, plesiosauria. Jurassic, devon, dorset, blue lias, charmouth mudstone, correlation. For all specimens the geological horizon from which the ammonites were derived was carefully identified. To the east of staithes, you can see the higher part of the staithes formation in the lower part of the cliff and the higher beds of the cleveland ironstone formation. Microstructural controls on the uredependent press permeability of whitby mudstone rosanne mckernan 1, julian mecklenburgh, ernie rutter and kevin taylor. Mudstone is made up of finegrained clay particles whitby mudstone formation wmf is a finegrained mudstone with siltsized minerals embedded in a finegrained matrix, which is microstructurally comparable to the psf. It overlies the preceding northampton sand formation and underlies the following lincolnshire limestone. Impact of water saturation on the elastic anisotropy of. Feb 14, 20 the pliensbachiantoarcian early jurassic fossil record is an archive of natural data of benthic community response to global warming and marine longterm hypoxia and anoxia.
Falciferumbifrons in regional chronostratigraphy geological formation in yorkshire and worcestershire, england. Dogger formation dogger ironstone limestonesandstone lias group cleveland ironstone fm whitby mudstone fm. Challenges and requirements jonathan gammon head of ground investigations, hs2 ltd geotechnica 2015. Further up the coast, to the north of staithes, both saltburn and redcar also have excellent. The whitby mudstone formation has large clay content, which in turn forms the lowest resistivities at site 10. The whitby mudstone formation has been divided into five members rawson and wright 1995, the middle of which is the alum shale member formerly the alum shale series. The whitby mudstone formation is an analogue for the dutch posidonia shale which was deposited during the early toarcian, and is a possible unconventional gas source in nor thern europe. Acoustic emissions aes monitoring is also performed between any two consecutive surveys.
1456 602 1237 1197 311 710 129 278 1194 54 583 753 1106 616 755 438 483 447 1161 321 1554 852 1292 504 1009 387 621 1033 1359 1327 447 743 652 1445 591 1067 701 96 1419