Advanced NMR methodologies in rock core analysis
0 sources
Advanced NMR methodologies in rock core analysis
Summary
Advanced NMR methodologies in rock core analysis is a doctoral thesis[1].
Key Facts
- Advanced NMR methodologies in rock core analysis authored Huabing Liu[2].
- Advanced NMR methodologies in rock core analysis's instance of is recorded as doctoral thesis[3].
- Advanced NMR methodologies in rock core analysis was published by Open Access Repository Victoria University of Wellington[4].
- Advanced NMR methodologies in rock core analysis's language of work or name is recorded as English[5].
- Advanced NMR methodologies in rock core analysis's country of origin is recorded as New Zealand[6].
- Advanced NMR methodologies in rock core analysis was published on January 1, 2015[7].
- Advanced NMR methodologies in rock core analysis's main subject is nuclear magnetic resonance[8].
- Advanced NMR methodologies in rock core analysis's main subject is magnetic resonance imaging[9].
- Advanced NMR methodologies in rock core analysis's title is recorded as Advanced NMR methodologies in rock core analysis[10].
- Advanced NMR methodologies in rock core analysis's copyright holder is recorded as Huabing Liu[11].
- Advanced NMR methodologies in rock core analysis's thesis submitted to is recorded as Victoria University of Wellington[12].
- Advanced NMR methodologies in rock core analysis's on focus list of Wikimedia project is recorded as NZThesisProject[13].
- Advanced NMR methodologies in rock core analysis's copyright status is recorded as copyrighted[14].
- Advanced NMR methodologies in rock core analysis's thesis committee member is recorded as Petrik Galvosas[15].
- Advanced NMR methodologies in rock core analysis's thesis committee member is recorded as Robin Dykstra[16].
- Advanced NMR methodologies in rock core analysis's thesis submitted for degree is recorded as Doctor of Philosophy[17].
Body
Designation and Status
Advanced NMR methodologies in rock core analysis's instance of is recorded as doctoral thesis[3].