View Triples for http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter

In-coming triples
Subject	Predicate	Object	Graph	Adapter
http://www.cidoc-crm.org/extensions/crmsci/O23_is_defined_by	http://www.w3.org/2000/01/rdf-schema#domain	http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter	https://nfdi4objects.wisski.data.fau.de/sites/default/files/ontology/CRMsci_v2.0.owl	Default WissKI Distillery Adapter
http://www.cidoc-crm.org/extensions/crmarchaeo/AP10_destroyed	http://www.w3.org/2000/01/rdf-schema#range	http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter	https://nfdi4objects.wisski.data.fau.de/sites/default/files/ontology/CRMarchaeo_v2.1.1.owl	Default WissKI Distillery Adapter
http://www.cidoc-crm.org/extensions/crmarchaeo/AP10i_was_destroyed_by	http://www.w3.org/2000/01/rdf-schema#domain	http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter	https://nfdi4objects.wisski.data.fau.de/sites/default/files/ontology/CRMarchaeo_v2.1.1.owl	Default WissKI Distillery Adapter
http://www.cidoc-crm.org/extensions/crmsci/O23i_defines	http://www.w3.org/2000/01/rdf-schema#range	http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter	https://nfdi4objects.wisski.data.fau.de/sites/default/files/ontology/CRMsci_v2.0.owl	Default WissKI Distillery Adapter

Out-going triples
Subject	Predicate	Object	Graph	Adapter
http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter	http://www.w3.org/1999/02/22-rdf-syntax-ns#type	http://www.w3.org/2002/07/owl#Class	https://nfdi4objects.wisski.data.fau.de/sites/default/files/ontology/CRMsci_v2.0.owl	Default WissKI Distillery Adapter
http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter	http://www.w3.org/2004/02/skos/core#notation	"S22"	https://nfdi4objects.wisski.data.fau.de/sites/default/files/ontology/CRMsci_v2.0.owl	Default WissKI Distillery Adapter
http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter	http://www.w3.org/2004/02/skos/core#prefLabel	"Segment of Matter"@en	https://nfdi4objects.wisski.data.fau.de/sites/default/files/ontology/CRMsci_v2.0.owl	Default WissKI Distillery Adapter
http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter	http://www.w3.org/2000/01/rdf-schema#subClassOf	http://www.cidoc-crm.org/extensions/crmsci/S20_Rigid_Physical_Feature	https://nfdi4objects.wisski.data.fau.de/sites/default/files/ontology/CRMsci_v2.0.owl	Default WissKI Distillery Adapter
http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter	http://www.w3.org/2000/01/rdf-schema#comment	"Scope note: This class comprises physical features with relative stability of form and structure within a declared spatial volume of interest. The spatial extent of an instance of S22 Segment of Matter may be declared or defined by a researcher or observer usually because the arrangement and composition of substance is characteristic for the surrounding matter or can be interpreted as traces of its genesis and subsequent internal and external processes it was exposed to. The defining spatial extent is typically declared on a continuous matter by means of geometric determination without observable boundaries on all sides or any side. It may however be extracted at some point in time along the declared boundaries. An instance of S22 Segment of Matter is regarded to be existing from the time on it completely solidified with a structure that is still preserved in a recognizable way at the time of its spatial definition. Its existence is regarded to end when its respective integrity is partially or completely corrupted. Uncorrupted subsections of an instance of S22 Segment of Matter may continue to exist as segments of matter in their own right beyond the existence of the containing instance, and may have solidified before it. Typical examples are segments of archaeological or geological layers. They are regarded as uncorrupted even if they have undergone conformal deformations, such as compressions or shifts, as long as the effects of these deformations do not destroy the relevant structures of interest. This means that the defining spatial volume may be only geometrically valid for an instant of time for which it was declared, and undergo before and after deformations. In some cases, it may be possible to calculate the initial volume at the time of solidification, for instance for petrified bones compressed in Jurassic layers. Examples: - the clay floor A11 [Heterogeneous, yellow to grey silty clay; clear, wavy lower boundary] (illu p. 1601, Croix et al, 2019) In First Order Logic: - S22(x) ⇒ S20(x) "@en	https://nfdi4objects.wisski.data.fau.de/sites/default/files/ontology/CRMsci_v2.0.owl	Default WissKI Distillery Adapter
http://www.cidoc-crm.org/extensions/crmsci/S22_Segment_of_Matter	http://www.w3.org/2000/01/rdf-schema#label	"S22 Segment of Matter"@en	https://nfdi4objects.wisski.data.fau.de/sites/default/files/ontology/CRMsci_v2.0.owl	Default WissKI Distillery Adapter