Intrusion

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INTRUSION, estates, torts. When an ancestor dies seised of an estate of inheritance expectant upon an estate for life, and then the tenant dies, and between his death and the entry of the heir, a stranger unlawfully enters upon the estate, this is called an intrusion. It differs from an abatement, for the latter is an entry into lands void by the death of a tenant in fee, and an intrusion, as already stated, is an entry into land void by the death of a tenant for years. F. N. B. 203 3 Bl. Com. 169 Archb. Civ. Pl. 12; Dane's Ab. Index, h. t.

INTRUSION, remedies. The name of a writ, brought by the owner of a fee simple, &c., against an intruder. New Nat. Br. 453.

A Law Dictionary, Adapted to the Constitution and Laws of the United States. By John Bouvier. Published 1856.
References in periodicals archive ?
Most of the NW-SE fractures are filled with barite and less commonly, lead-zinc ores, and their predominance in the intrusive rocks suggests that they are probably Post-Santonian in age.
The aim of this study is to present new Sr and Nd isotopic data from some intrusive rocks of Laramide Arc to discuss their geochemistry, age, different magmas relationship, and the role and type of basement involved.
In addition, there are two undeformed, unmetamorphosed, intrusive rocks with U-Pb LA-ICPMS zircon ages of 48.1 +-0.8 Ma and 45.8 +-0.8 Ma.
The lithology of intrusive rocks consists of gabbro, diorite, quartz diorite, granodiorite, biotite granite and leucogranite.
According to the current New Brunswick lexicon of bedrock geology (New Brunswick Department of Natural Resources 2010), the Saint George Plutonic Suite is a contiguous cluster of mainly high-level intrusive rocks comprising (in inferred chronological order from oldest to youngest) the Bocabec Gabbro, Utopia Granite, Welsford,Jake Lee Mountain, and Parks Brook alkali granites, Magaguadavic Granite, John Lee Brook Granite, and Mount Douglas Granite.
He studied ferromagnesian minerals in the basic igneous intrusive rocks in the Wichita Mountains of Oklahoma.
Vermiculite mineralization in the Agasthyapura area occurs within the ultramafic body which trends in N35[degrees]E direction and at the contact zones between the N65[degrees]E trending and dipping subvertical acid (felsic) intrusive rocks. The vermiculite accumulations occur as clots within the ultramafic body and also as narrow belts, found in the marginal portions of fractured and altered ultramafic rocks in contact with acid intrusive (Fig.
Intrusive rocks of the Coldwell Complex revealed high grade mineral zones of copper, gold, palladium and platinum and other metals.
and Desborough, G.A., 1970, Mafic intrusive rocks of Precambrian age in southeast Missouri, Missouri Division of Geology and Land Survey, Report of Investigations 47.