Natural bitumens in kimberlite pipes and host rocks in the Yakutian diamond province
Natural bitumens in kimberlite pipes and host rocks in the Yakutian diamond province
Russian Geology and Geophysics (2005) 46 (2): 148-158
- Aldan Shield
- Anabar Shield
- aromatic hydrocarbons
- Asia
- asphalt
- bitumens
- Commonwealth of Independent States
- crude oil
- Devonian
- diamond deposits
- geochemistry
- heating
- hydrocarbons
- igneous rocks
- inclusions
- infrared spectra
- intrusions
- kimberlite
- Lena Basin
- lower Paleozoic
- naphthalene
- Neoproterozoic
- Olenek River
- organic compounds
- Paleozoic
- petroleum
- petroleum accumulation
- pipes
- polycyclic aromatic hydrocarbons
- Precambrian
- Proterozoic
- Russian Federation
- Siberian Platform
- source rocks
- spectra
- stability
- temperature
- thermal properties
- Tunguska Basin
- upper Precambrian
- xenoliths
- Yakutia region
- Yakutia Russian Federation
Natural bitumens are widespread in the sedimentary cover of the Yakutian diamond province. They occur within a broad stratigraphic range and differ in size and character. A number of oil and gas fields have been discovered in the province. Numerous natural bitumen occurrences are found in kimberlite pipes and host rocks. Geochemical characteristics of the samples taken from different sites in and off the body of kimberlite pipe - kimberlite, xenolith, host rocks - display a rather intricate pattern. Their composition can be considered as a result of superposition of two processes: thermal destruction and deasphaltization of oils. The calculated temperatures of host rock heating and the time of cooling of kimberlite pipe suggest weak thermal destruction in both xenoliths and host rocks.