Interbedded is an English word. Below you'll find 2 example sentences showing how it's used in practice.
Interbedded in a sentence
Interbedded meaning
Occurring between beds of rock.
Using Interbedded
- The main meaning on this page is: Occurring between beds of rock.
Context around Interbedded
- Average sentence length in these examples: 26.5 words
- Position in the sentence: 0 start, 1 middle, 1 end
- Sentence types: 2 statements, 0 questions, 0 exclamations
Corpus analysis for Interbedded
- In this selection, "interbedded" usually appears in the middle of the sentence. The average example has 26.5 words, and this corpus slice is mostly made up of statements.
- Around the word, pelitic stand out and add context to how "interbedded" is used.
- Recognizable usage signals include are found interbedded with glacial and quartzite and interbedded pelitic biotite. That gives this page its own corpus information beyond isolated example sentences.
- By corpus frequency, "interbedded" sits close to words such as aabc, aacr and aacsb, which helps place it inside the broader word index.
Example types with interbedded
The same corpus examples are grouped by length and sentence type, making it easier to see the contexts in which the word appears:
A further difficulty in suggesting that BIFs marked the end of the glaciation is that they are found interbedded with glacial sediments. (22 words)
Gold mineralization is hosted within a meta-sedimentary sequence dominated by banded (graphitic) quartzite and interbedded pelitic biotite schist that is cross-cut by numerous felsic to intermediate dikes and sills. (31 words)
Gold mineralization is hosted within a meta-sedimentary sequence dominated by banded (graphitic) quartzite and interbedded pelitic biotite schist that is cross-cut by numerous felsic to intermediate dikes and sills. (31 words)
A further difficulty in suggesting that BIFs marked the end of the glaciation is that they are found interbedded with glacial sediments. (22 words)
Example sentences (2)
Gold mineralization is hosted within a meta-sedimentary sequence dominated by banded (graphitic) quartzite and interbedded pelitic biotite schist that is cross-cut by numerous felsic to intermediate dikes and sills.
A further difficulty in suggesting that BIFs marked the end of the glaciation is that they are found interbedded with glacial sediments.