Keywords: 
• Sichuan Basin

Abstract: In recent years, much more tightgas of the late Triassic Xujiahe Formation are discovered in Yuanba which  is located in the northeastern  Sichuan foreland basin in China, Sichuan Basin is about 1.9×106 km2 that evolved into foreland basin from Paleozoic platform in late Triassic. The basin is surrounded by the Longmen thrust belt(west), Jiangnan uplift(east),MichangDaba thrust belt(north) and Kangdian uplift(south). The provenance of Yuanba sedimentary rock come from Michang thrust belt, and the main sedimentary types are nonmarine braided delta and shallow lake Facies in Xujiahe Formation that can be divided into 5 rock section, Tx1, Tx3, Tx5 is shallow lake mudsiltstone and lateral continues, Tx2,Tx4 are sandstones deposited by braided river delta. Braided channels sandstones are developed extremely and overlap each other in vertical and continuous distribution. These characters are similar to the other areas of Sichuan basin.
  But quartz sandstones are found first in the upper Triassic Xujiahe Formation in Sichuan basin. Quartz sandstones are distributed at the bottom of Tx1 and interlayer Tx2 of Xujiahe in Yuanba, these quartz sandstones occurrence is particular that occur in unconformable surface of Tx1 and on the top of two layers lithic arenites of Tx2 that are composed of three rock section(Tx
12 sandstone, Tx12 mudsiltstone and Tx32 sandstone). Results of our study point out that quartz sandstones are different depositional environment from lithic sandstones below which belong to deltaic deposits widely in highstand and early regressive systems tracts, whereas quartz sandstones are deposited in beach or tidal  environment when the sea level rise rapidly, our analysis shows that quartz sandstones beach are long and narrow parallel to shoreline, and may be controlled by Michang Mount foredeep belt, but lithic sandstones braided delta below extend from north to south perpendicular to shoreline. 
  Quartz arenites are easily recognized with lower GR log than other sandstones, and mainly very fine sands(Tx1) to fine sands(Tx2) with little clay or matrix grains, and have mature compositional and textural maturity. Quartz sandstones thickness is about 10 to 15 m in the study area.
  Because of strong digenesis process(Mesogenesis to Telogenesis), Xujiahe sandstones are tightgas reservoir with porosity ranging from 5.0%~11.0% and average permeability 1.9×10-3μm2. According to much more casting thinsection, the primary pores little occur in all kinds of sandstones. The secondary pores are major pore types that come from dissolution of minerals and fragments. Generally there
are  a  few  quartz sandstones reservoirs developed in Xujiahe Fm.  but they have better reservoir conditions in Yuanba area because high density protogenetic fissure are developed in quartz grains of quartz sandstones, and these protogenetic fissure may be closed in diagenetic processes after deposition. When tectonic extrusion stress occur, new much fissures are produced and old reopened in quartz sandstones because quartz sandstones with cracks are easily broken, and immensely increase cracks density. Meanwhile,  these fissures also induce a lot of dissolution process that improve porosity and connectivity of quartz sandstones reservoirs. According to casting thinsections, the main pore types of quartz sandstones are fissures that include long newborn cracks and short protogenetic cracks, and the secondly pore types are corrosion pores that distributed along fractures.
  Our analysis shows quartz sandstones as reservoirs related to provenance come from Michang thrust belt, quartz grains with cracks are not only in quartz sandstones, but also other kinds of sandstones for example lithic sandstones have quartz mineral with cracks in Yuanba area, so crack quartz maybe come from ancient source rocks.