$0.00
2-3 Rasmussen, J.C., Keith, S.B., Swan, M.M., Laux, D. P., and Caprara, J., 2003, Strike-slip faulting and reservoir development in New York State: New York State Energy Research and Development Authority, Albany, NY, Contract Agreement no. 6984, 161 p.
ABS
This study of tectonics and reservoir development at and near Glodes Corner, New York, has led to the development of an integrative hydrothermal dolomite (HTD) gas exploration model that not only has the potential to define gas or oil accumulations, but also may define important internal conduit features that are related to the hydrocarbon charge. The Glodes Corner field is characterized by a seismically defined sag structure that reflects a collapse feature associated with the formation of HTD at the Trenton-Black River level that is some 8,000 feet below the surface. Soil geochemistry interpreted according to this new fluid fractionation and shear-system kinematic model identifies well-developed, east-to-west asymmetrical patterns in redox potential (CO2:O2 and ferrous:ferric ratios) and the distribution and compositional mixtures of hydrocarbon gases and a variety of trace metals.
2-3 Rasmussen, J.C., Keith, S.B., Swan, M.M., Laux, D. P., and Caprara, J., 2003, Strike-slip faulting and reservoir development in New York State: New York State Energy Research and Development Authority, Albany, NY, Contract Agreement no. 6984, 161 p.
ABS
This study of tectonics and reservoir development at and near Glodes Corner, New York, has led to the development of an integrative hydrothermal dolomite (HTD) gas exploration model that not only has the potential to define gas or oil accumulations, but also may define important internal conduit features that are related to the hydrocarbon charge. The Glodes Corner field is characterized by a seismically defined sag structure that reflects a collapse feature associated with the formation of HTD at the Trenton-Black River level that is some 8,000 feet below the surface. Soil geochemistry interpreted according to this new fluid fractionation and shear-system kinematic model identifies well-developed, east-to-west asymmetrical patterns in redox potential (CO2:O2 and ferrous:ferric ratios) and the distribution and compositional mixtures of hydrocarbon gases and a variety of trace metals.
Zonal patterns identified within the field conform to an inferred reaction sequence that follows two earlier stages. Stage 1 is generation of methane/hydrocarbon-stable, metagenic fluids formed by serpentinization of peridotite in intracratonic failed rifts or collisional sutures in the basement as triggered by compressive, convergent orogenesis. Stage 2 is initial, low temperature, ‘passive’ dolomitization of the first replaceable, typically shelf carbonate in the overlying cratonic cover sequence. The following paragenetic stages occur at the reservoir site: Stage 3A (early saddle dolomitization at or near the depositional site), Stage 3B (late saddle dolomitization, anhydrite formation, carbon dioxide effervescence, hydrogen loss and methane unmixing), Stage 4 (sulfide and hydrocarbon deposition), and Stage 5 (deposition of late calcite at the depositional site and illite/smectite/kaolinite clays in and marginal to the depositional site).
This paragenetic reaction series is the predicted fractionation pattern developed from an initially reduced, high-temperature fluid evolving toward a more oxidized, lower-temperature fluid. The within-reservoir, conduit architecture of permeability and dolomite permeability plugging can be identified by interpretation of hydrocarbon gas distribution (C1-C2 high in conduits) and trace metal distribution (elevated along with C5 and C6 hydrocarbons away from the conduits). By integrating soil gas geochemistry, fluid fractionation, and shear-system kinematics, it may be possible to precisely detect permeable conduits inside the resolution from seismic imaging. This model has significant exploration implications for the geochemical identification of hydrocarbon-charged reservoirs where combined structural and stratigraphic features have produced geochemically zoned, three-dimensional geographic patterns during emplacement of the hydrocarbon charge.
The Glodes Corner field is located in the northeasternmost part of Steuben County in south-central New York. Glodes Corner is the largest of a cluster of gas fields hosted in hydrothermal dolomites that have replaced shelf limestones in the Upper Ordovician Trenton-Black River Groups beneath south-central New York. Glodes Corner has sufficient hydrocarbons to be ranked as a ‘significant’ gas field in the U.S. Geological Survey classification. The field itself occurs beneath a seismically defined sag feature that is expressed at the current topographic surface as an east-northeast-striking synclinal fold in Devonian strata within the Catskill delta wedge. The Catskill wedge is the main sedimentological feature of the Acadian Orogeny of Devonian age and formed in its foreland.
During the Acadian Orogeny (350-400 Ma), large-scale, basement-derived, possibly hydrocarbon-stable, hydrothermal fluids are thought to have been derived from a serpentinized peridotite source in the Cambrian-age rift system beneath central Steuben County, New York. The inferred serpentine source is consistent with a prominent magnetic feature (resulting from magnetite formed during serpentinization) that coincides with a conspicuous gravity low in the middle of the magnetic high (resulting from low density serpentine). Serpentinization of the inferred peridotite is thought to have accompanied greenschist grade (~300˚C at 5-8 km depth) metamorphism and the rift basement during the peak Acadian  metamorphic event at about 360-375 Ma.
Hydrothermal fluids originating from the inferred peridotitic source are thought to have utilized a conduit system consisting of interconnected northwest- and northeast- to east-northeast-striking faults to travel from the serpentinized source to the Trenton-Black River shelf carbonate cover sequence. At Glodes Corner, potentially hydrocarbon-stable, hydrothermal, low-pH, carbonated alkali brines are thought to have laterally and vertically ascended along a N50W-striking feeder-conduit. Both vitrinite reflectance and conodont alteration index data indicate that the deep gas cluster in south-central New York could have formed in the uppermost part of or even above the thermogenic gas window, which is 200Ëš to 300ËšC.
At Glodes Corner, the fluids migrated westward into an incipient riedel/tensile structural trap in highly reactive and replaceable calcitic limestones of the Trenton-Black River cratonic shelf cover. East-to-west flow is consistent with a gradual west-tapering within the field, which is about 5 km long in an east-west direction. The structural setting predicted an east-to-west chemical fractionation. A chemical zonation pattern resulted from fractionation of fluids that deposited a high-temperature, reduced chemical assemblage at the east end and deposited lower temperature, more oxidized distillates at its western end near the tip of the inferred fluid/alteration wedge. In particular, the zonal patterns at Glodes Corner strongly conform to the portion of the reaction sequence covered by stages 3A (early saddle dolomitization at and near depositional site) and 3B (late saddle dolomitization, anhydrite formation, carbon dioxide effervescence, hydrogen loss and methane unmixing), stage 4 (sulfide deposition and hydrocarbon deposition), and stage 5 (deposition of late calcite at depositional site and illite/ smectite/ kaolinite clays in and marginal to depositional site).
Subsequent to the emplacement of the gas-bearing hydrothermal deposit, south-central New York was affected by the north-northwest – south-southeast shortening associated with the Alleghenian orogeny at about 260 to 300 Ma. At this time, the reservoir and the overlying Catskill sedimentary wedge were deformed around east-northeast – west-southwest-trending, broad, fold warps in the northern part of theAlleghenian fold-thrust deformational fan in the Pennsylvanian embayment/salient. Location of the fold features may have, in part, been controlled by the antecedent, Acadian–produced, riedel/tensile, graben/sag features, such as that at Glodes Corner.
Fluid migration patterns in strike-slip settings hosting hydrothermal metalliferous system (Carlin-type gold deposits) are analogous to hydrocarbon migration patterns, particularly in hydrothermal dolomite settings. Faults are not merely passive conduits and seals that statically receive and trap fluid sometime after their formation. Rather, fluid formation, movement, and deposition within any fault system characterize an active process that co-dynamically conjoins fault kinematics with fluid generation, flow, and deposition.
Porphyry metal deposit analogs (Carlin/North Trend of Nevada) indicate a synkinematic relationship between strike-slip fault movements, the emplacement of pluton gold sources, and the release of gold-bearing fluids into riedel/tensile splays and/or wedge-like stratigraphic traps. The most economic traps involve the intersection of favorable stratigraphy with the footwall of P-shear conduits. Where this stratigraphy is blocked in its updip portions by other faults that mark changes in dip domain or juxtapositions with unfavorable stratigraphy, a wedge-like ‘trap’ can be associated with especially high grade gold accumulations (e.g., Meikle mine). The fluid migration path is identified through geochemistry. As fluids migrate from a high pressure source to low pressure deposition sites, they fractionate, resulting in a systematic paragenetic chemical dispersal sequence. Increase in oxidation state during the process is a first order control on the fractionation.
Similar strike-slip configurations trap accumulations of petroleum in strike-slip fault environments (Jonas and Cave Creek gas fields in Wyoming and Glodes Corner, Steuben County, New York). In both mineral deposit and petroleum systems, the paths of the economic fluids utilized a curved trajectory in moving from the P-shear conduit to the stratigraphic wedge. This curved trajectory appears to be characteristic of fluid migration in both porphyry metal and petroleum accumulations related to wrench-fault tectonism.
Recent geochemical data from Glodes Corner, New York, may define fluid migration pathways that are analogous to the fluid migration pathways in Carlin gold systems. Carbon geochemistry fractionates from west to east along the riedel/tensile conduit. This fluid pathway is inferred from the presence of a more H-rich, reduced assemblage of higher CO2/O2 ratios, C-1 to C-4 gases on the east (near the intersection with an inferred northwest-trending ‘feeder’ structure) to a more oxidized, H -poor environment on the west, characterized by and assemblage of higher C-number gases (especially C-5 and C-6) and more oxidized, O-rich assemblage characterized by lower CO2/O2 ratios on the west. The inferred feeder structure appears to have been undergoing active, left-slip kinematics at the time of the gas introduction, which is inferred to have entered the hydrothermal dolomite reservoir in the underlying Trenton/Black River section from the southeast. Fluid movement and its fractionation are necessary products of interactively coordinated kinematics within the strike-slip fault system and, more importantly, specifically predict economic targets.
| Book Format | Print to Order, Digital Version |
|---|
2-3 Rasmussen, J.C., Keith, S.B., Swan, M.M., Laux, D. P., and Caprara, J., 2003, Strike-slip faulting and reservoir development in New York State: New York State Energy Research and Development Authority, Albany, NY, Contract Agreement no. 6984, 161 p.
ABS
This study of tectonics and reservoir development at and near Glodes Corner, New York, has led to the development of an integrative hydrothermal dolomite (HTD) gas exploration model that not only has the potential to define gas or oil accumulations, but also may define important internal conduit features that are related to the hydrocarbon charge. The Glodes Corner field is characterized by a seismically defined sag structure that reflects a collapse feature associated with the formation of HTD at the Trenton-Black River level that is some 8,000 feet below the surface. Soil geochemistry interpreted according to this new fluid fractionation and shear-system kinematic model identifies well-developed, east-to-west asymmetrical patterns in redox potential (CO2:O2 and ferrous:ferric ratios) and the distribution and compositional mixtures of hydrocarbon gases and a variety of trace metals.
Zonal patterns identified within the field conform to an inferred reaction sequence that follows two earlier stages. Stage 1 is generation of methane/hydrocarbon-stable, metagenic fluids formed by serpentinization of peridotite in intracratonic failed rifts or collisional sutures in the basement as triggered by compressive, convergent orogenesis. Stage 2 is initial, low temperature, ‘passive’ dolomitization of the first replaceable, typically shelf carbonate in the overlying cratonic cover sequence. The following paragenetic stages occur at the reservoir site: Stage 3A (early saddle dolomitization at or near the depositional site), Stage 3B (late saddle dolomitization, anhydrite formation, carbon dioxide effervescence, hydrogen loss and methane unmixing), Stage 4 (sulfide and hydrocarbon deposition), and Stage 5 (deposition of late calcite at the depositional site and illite/smectite/kaolinite clays in and marginal to the depositional site).
This paragenetic reaction series is the predicted fractionation pattern developed from an initially reduced, high-temperature fluid evolving toward a more oxidized, lower-temperature fluid. The within-reservoir, conduit architecture of permeability and dolomite permeability plugging can be identified by interpretation of hydrocarbon gas distribution (C1-C2 high in conduits) and trace metal distribution (elevated along with C5 and C6 hydrocarbons away from the conduits). By integrating soil gas geochemistry, fluid fractionation, and shear-system kinematics, it may be possible to precisely detect permeable conduits inside the resolution from seismic imaging. This model has significant exploration implications for the geochemical identification of hydrocarbon-charged reservoirs where combined structural and stratigraphic features have produced geochemically zoned, three-dimensional geographic patterns during emplacement of the hydrocarbon charge.
The Glodes Corner field is located in the northeasternmost part of Steuben County in south-central New York. Glodes Corner is the largest of a cluster of gas fields hosted in hydrothermal dolomites that have replaced shelf limestones in the Upper Ordovician Trenton-Black River Groups beneath south-central New York. Glodes Corner has sufficient hydrocarbons to be ranked as a ‘significant’ gas field in the U.S. Geological Survey classification. The field itself occurs beneath a seismically defined sag feature that is expressed at the current topographic surface as an east-northeast-striking synclinal fold in Devonian strata within the Catskill delta wedge. The Catskill wedge is the main sedimentological feature of the Acadian Orogeny of Devonian age and formed in its foreland.
During the Acadian Orogeny (350-400 Ma), large-scale, basement-derived, possibly hydrocarbon-stable, hydrothermal fluids are thought to have been derived from a serpentinized peridotite source in the Cambrian-age rift system beneath central Steuben County, New York. The inferred serpentine source is consistent with a prominent magnetic feature (resulting from magnetite formed during serpentinization) that coincides with a conspicuous gravity low in the middle of the magnetic high (resulting from low density serpentine). Serpentinization of the inferred peridotite is thought to have accompanied greenschist grade (~300˚C at 5-8 km depth) metamorphism and the rift basement during the peak Acadian  metamorphic event at about 360-375 Ma.
Hydrothermal fluids originating from the inferred peridotitic source are thought to have utilized a conduit system consisting of interconnected northwest- and northeast- to east-northeast-striking faults to travel from the serpentinized source to the Trenton-Black River shelf carbonate cover sequence. At Glodes Corner, potentially hydrocarbon-stable, hydrothermal, low-pH, carbonated alkali brines are thought to have laterally and vertically ascended along a N50W-striking feeder-conduit. Both vitrinite reflectance and conodont alteration index data indicate that the deep gas cluster in south-central New York could have formed in the uppermost part of or even above the thermogenic gas window, which is 200Ëš to 300ËšC.
At Glodes Corner, the fluids migrated westward into an incipient riedel/tensile structural trap in highly reactive and replaceable calcitic limestones of the Trenton-Black River cratonic shelf cover. East-to-west flow is consistent with a gradual west-tapering within the field, which is about 5 km long in an east-west direction. The structural setting predicted an east-to-west chemical fractionation. A chemical zonation pattern resulted from fractionation of fluids that deposited a high-temperature, reduced chemical assemblage at the east end and deposited lower temperature, more oxidized distillates at its western end near the tip of the inferred fluid/alteration wedge. In particular, the zonal patterns at Glodes Corner strongly conform to the portion of the reaction sequence covered by stages 3A (early saddle dolomitization at and near depositional site) and 3B (late saddle dolomitization, anhydrite formation, carbon dioxide effervescence, hydrogen loss and methane unmixing), stage 4 (sulfide deposition and hydrocarbon deposition), and stage 5 (deposition of late calcite at depositional site and illite/ smectite/ kaolinite clays in and marginal to depositional site).
Subsequent to the emplacement of the gas-bearing hydrothermal deposit, south-central New York was affected by the north-northwest – south-southeast shortening associated with the Alleghenian orogeny at about 260 to 300 Ma. At this time, the reservoir and the overlying Catskill sedimentary wedge were deformed around east-northeast – west-southwest-trending, broad, fold warps in the northern part of theAlleghenian fold-thrust deformational fan in the Pennsylvanian embayment/salient. Location of the fold features may have, in part, been controlled by the antecedent, Acadian–produced, riedel/tensile, graben/sag features, such as that at Glodes Corner.
Fluid migration patterns in strike-slip settings hosting hydrothermal metalliferous system (Carlin-type gold deposits) are analogous to hydrocarbon migration patterns, particularly in hydrothermal dolomite settings. Faults are not merely passive conduits and seals that statically receive and trap fluid sometime after their formation. Rather, fluid formation, movement, and deposition within any fault system characterize an active process that co-dynamically conjoins fault kinematics with fluid generation, flow, and deposition.
Porphyry metal deposit analogs (Carlin/North Trend of Nevada) indicate a synkinematic relationship between strike-slip fault movements, the emplacement of pluton gold sources, and the release of gold-bearing fluids into riedel/tensile splays and/or wedge-like stratigraphic traps. The most economic traps involve the intersection of favorable stratigraphy with the footwall of P-shear conduits. Where this stratigraphy is blocked in its updip portions by other faults that mark changes in dip domain or juxtapositions with unfavorable stratigraphy, a wedge-like ‘trap’ can be associated with especially high grade gold accumulations (e.g., Meikle mine). The fluid migration path is identified through geochemistry. As fluids migrate from a high pressure source to low pressure deposition sites, they fractionate, resulting in a systematic paragenetic chemical dispersal sequence. Increase in oxidation state during the process is a first order control on the fractionation.
Similar strike-slip configurations trap accumulations of petroleum in strike-slip fault environments (Jonas and Cave Creek gas fields in Wyoming and Glodes Corner, Steuben County, New York). In both mineral deposit and petroleum systems, the paths of the economic fluids utilized a curved trajectory in moving from the P-shear conduit to the stratigraphic wedge. This curved trajectory appears to be characteristic of fluid migration in both porphyry metal and petroleum accumulations related to wrench-fault tectonism.
Recent geochemical data from Glodes Corner, New York, may define fluid migration pathways that are analogous to the fluid migration pathways in Carlin gold systems. Carbon geochemistry fractionates from west to east along the riedel/tensile conduit. This fluid pathway is inferred from the presence of a more H-rich, reduced assemblage of higher CO2/O2 ratios, C-1 to C-4 gases on the east (near the intersection with an inferred northwest-trending ‘feeder’ structure) to a more oxidized, H -poor environment on the west, characterized by and assemblage of higher C-number gases (especially C-5 and C-6) and more oxidized, O-rich assemblage characterized by lower CO2/O2 ratios on the west. The inferred feeder structure appears to have been undergoing active, left-slip kinematics at the time of the gas introduction, which is inferred to have entered the hydrothermal dolomite reservoir in the underlying Trenton/Black River section from the southeast. Fluid movement and its fractionation are necessary products of interactively coordinated kinematics within the strike-slip fault system and, more importantly, specifically predict economic targets.
Alfredboold
A plataforma BitPreço, que não é exatamente uma exchange, mas um marketplace de criptomoedas, começou em 2018 e hoje coloca usuários em contato com diversas corretoras, nacionais e internacionais. O preço mais atual por um Game Coin (GMEX) é $0.00103. Atualizamos o preço Game Coin Cripto em tempo real. O Axie Infinity, por exemplo, que foi um jogo que explodiu neste ano teve o seu token valorizado em mais de 59.000%. Isso significa que, um usuário que adquiriu ativos do gamecoin em julho teve no mês de setembro uma valorização de 1.055,67%. CGC foi adicionado por menos de três meses e tem uma classificação baixa em 3718 no CoinMarketCap, prevemos que o preço e a capitalização de mercado desta moeda serão muito voláteis e os comerciantes devem ser extremamente cautelosos ao investir em CGC . É possÃvel que essa moeda suba drasticamente, embora seja igualmente provável que caia pesadamente. Portanto, tome cuidado e invista apenas no que está disposto a perder. http://raymondoiyp643108.win-blog.com/14765415/bitcoins-e-seguro-investir Por mais que o tema seja uma novidade, não é de hoje que o Banco Central estuda uma nova moeda. Em agosto do ano passado, o BC criou um grupo para estudar as moedas digitais emitidas por Bancos Centrais, ou os chamados Central Bank Digital Currency, e assim avaliar os benefÃcios e os impactos que poderiam vir com a criação de um real em formato digital. Pode parecer repetitivo, porém os destaques do Ethereum seguem sendo relativos à s melhorias do protocolo com as implementações do Casper e do Sharding. Hoje, aliás, Vitalik Buterin publicou uma nova proposta de melhoria para o protocolo no que se refere à s taxas de transação da rede. Vamos analisar com calma e manteremos nossos leitores informados. No ano passado, a China declarou ilegal todas as transações financeiras realizadas com criptomoedas. A decisão foi tomada, de acordo com o governo, para frear a lavagem de dinheiro e arrecadação de fundos ilegais. O Banco Central da China afirmou que, durante os últimos anos, o comércio com criptomoedas alteraram a ordem econômica e financeira, aumentando a lavagem de dinheiro, esquemas de pirâmides e demais atividades criminosas.
ThillKiB
These transactions are fully anonymous, secure, and are not beholden to central banks, intermediaries, or any other third parties. At a Bitcoin casino, you can simply use your mined or purchased Bitcoin (BTC), transfer ‘value’ to the online casino’s Bitcoin address and play ‘real-money’ casino games with no identifying criteria other than your Bitcoin address. An event betting platform with P2P odds generation. Bet for or against the odds on your favorite events and Multiply BTC. Live dealer games have been a big problem in online casinos for the past few years. The technology streams the action from a real casino and enables interaction between players and between players and the dealer. This allows the player to enjoy an immersive environment normally only found in a physical casino, all from the comfort of their own home. The best bitcoin casinos have the latest live technology and multiple tables to join and play the most popular casino games. Most live bitcoin casinos allow you to deposit a game so you can top up your balance at any time. Just make sure you know your cryptographic key or have access to your wallet before you start playing. https://major21.com/community/profile/rebecca79c6040/ Crypto free spin bonus and casino no deposit bonus are similar to other Bitcoin bonuses, where the intent is to entice and drive players to play. When it comes to online playing networks, it’s no secret that there’s a lot of competition. As a result, in an effort to surpass each other, such no deposit bonuses are offered to entice gamblers to pick a certain site. As a result, gamblers have a chance to win money without risking their own money. Whether a novice or a seasoned player, the preceding tips and methods should assist anyone experience the world of slot games and crypto casinos and win free spin at a crypto casino. In 2022 the importance of cryptocurrency is becoming clearer and clearer, and a white label casino is definitely not up to the standards without this payment option.
ThillKiB
JACKPOT WHEEL casino gives $40 free bonus no deposit to all new players that sign up and Redeem the code JACK40 Maximum cashout from winnings is set at $100 (or currency equivalent). In order to cashout from this bonus, a minimum deposit is required ($25). One claim per player only, no multiple accounts allowed. Two lucky ticketholders have won more than ВЈ2 million each in Saturday’s Lotto draw. Bonus designs vary between casinos. They are typically divided into two distinct types; Free Spins or a free amount of money. In both cases, they are used as welcome bonuses for new members, deposit bonuses you get after your first deposit or loyalty rewards for those who have been with a casino for some time. The first currency, sempre a buscar o lucro a longo prazo. Der Spielspaß, the small touch screen seems to be a disadvantage for online gambling players. Gambling sites not registered with gamstop i should do, not necessarily this kind of a suprisingly simple factor to do. This might be after the Swedish government finally realized just how many tax dollars are lost without a Swedish gaming license, switching boxes. And they aren’t happy about having been hacked, tic-tac-toe. On most maps you will find hidden Crew Challenges, Sudoku. https://www.theprintlife.com/community/profile/latiacrossley65/ Email sales@casinoquest.biz To prepare a group of diverse students seeking entry into beginning and supervisory positions in the casino industry by providing curriculum covering all aspects of casino operations including slots, table games, race and sports book operations, cage operations, surveillance, gaming laws, regulations, minimum internal control requirements, strategic management, and customer service standards. On every custom item, you will receive a FREE art proof on your order. Your inside sales representative will send your artwork to our professional artists who will make sure your imprint fits perfectly on the item you have chosen. We will not proceed with production until you are satisfied. No Download Casino Bonuses – The land-based casino crisis, the success of online slots
aball
Find out how we can help if you’re moving house. Learn about what you need to tell us when you move house and how it can affect your payments. You can also contact your local Citizens Information Centre. If you're moving in with your partner, have a chat about your finances. Get to know one another's attitude to money. Think about your financial goals, both short and long term. You don't have to have everything figured out, just start a conversation. If you're not sure where to start, you can use our free moving concierge to help you decide who to hire. We can help you find the best professional moving company, truck rental, moving container, and more! This guide lists the many resources that exist for New Yorkers looking for housing, such as rental assistance. It explains what Source of Income Discrimination is and how we can help. It also provides guidance on navigating the apartment search process. https://paxvox.com/community/profile/janetsmythe1579/ We have four plans to choose from, surely below your budget. When I moved to West Virginia, they picked up my car the very day I called them. I like to think they take special care of me considering all the business I’ve sent them. I’ll continue to support A1 Auto Transport. It’s my number one pick in auto shipping to this day. Even though we are a full service moving company, we understand that everyone has a budget so our movers will do as much or as little as you want them to. We understand that every move and every customer is different so we will do our best to keep the lines of communication open so that your move will go fast and smooth. You will have peace of mind, knowing that you are hiring the largest moving company in San Antonio that performs thousands of moves each year and we would be happy to answer any additional questions you may have regarding your upcoming move. Call 210-348-8199 for a fast and friendly moving estimate today.