Guide: How to cite a Patent in Myrmecological News style
Cite A Patent in Myrmecological News style
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Use the following template to cite a patent using the Myrmecological News citation style. For help with other source types, like books, PDFs, or websites, check out our other guides. To have your reference list or bibliography automatically made for you, try our free citation generator.
Key:
Pink text = information that you will need to find from the source.
Black text = text required by the Myrmecological News style.
Reference list
Place this part in your bibliography or reference list at the end of your assignment.
Template:
Author Surname, Author Initial. Year Published: Title. –
Example:
Eastern Solent Coastal Partnership, 2013: Southsea and North Portsea Island Coastal Flood and Erosion Risk Management Schemes. – : 29-29.
In-text citation
Place this part right after the quote or reference to the source in your assignment.
Template
(Author Surname Year Published)
Example
Group Stratum Bedrock Geology Quaternary Superficial Deposits Aeolian (Brickearth) Deposits Yellow/brown mainly non-calcareous silt or clayey silt which may locally contain a few flint and chalk fragments Alluvium Soft organic mottled silty and sandy clay Second River Terrace Gravels Gravels and sandy gravels (only the higher terraces are described as clayey). In the south of the Portsmouth district, the gravels are predominately flint Estuarine Alluvium Brown and grey mottled soft silty clay and silt Storm Gravel Beach Deposits Fine to medium gravels with some interstitial sand and shell debris Bracklesham Group Earnley Sand Formation Glauconitic silty sands and sandy silts, with thickness given as 22-25m. The Earnley Sand rests on the Wittering Formation, with the base of the Formation marked by the transgressive surface (a boundary formed by rapid sea level rise) overlain by glauconitic silty sands and pebble bed The Earnley Sand is overlain by the Marsh Farm Formation. The boundary is marked by the upward change from the Glauconitic Sands of the Earnley Sand Formation to the thin-bedded clays and silts with Glauconitic Sand laminae of the Marsh Farm Formation Marsh Farm Formation Laminated clay; sand interbedded with clay in equal proportions; and fine- to medium-grained sparsely Glauconitic Sand with laminae and intercalations of clay, with a thickness of 12 – 13.5m. As noted above, the formation rests on the Earnley Sand. It is overlain by the Selsey Sand Formation whose base is marked by a sharply change to thinly bedded clays and silts with glauconitic sand laminae. Wittering Formation Greyish brown laminated clay; sand interbedded with clay in equal proportions; and fine- to mediumgrained sparsely Glauconitic Sand. It rests on London Clay, a dark grey bioturbated clay and its thickness is given as 40-53m. The Wittering formation is overlain by Earnley Sand Formation, with the boundary marked by the transgressive basal surface of Glauconitic silty sands with pebbles Thames Group London Clay Formation Grey, pyritic, bioturbaded silty and fine-grained sandy clay with seams of calcareous cementstone and flint pebble beds. It has a sandy bed at the base Bognor Sand 5-10m thick and comprising Glauconitic bioturbated or cross-bedded fineand medium-grained sands, partially cemented Chalk Group Upper Chalk White chalk with flint seams Table 1. General Description of the lithology (Eastern Paretnership, 2012) (Eastern Solent Coastal Partnership 2013)
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